Create alert

Page1 ›FMRR‚Å—Z‰ð‘w‚ðˆµ‚¤A¢F~…Œ`¬‰ß’ö‚ðˆµ‚¤A~FŒ¸Š•â³A—±Œa•ª•z‚È‚Çi—Z‰ð‘wˆÈŠOj‚ª‘ÎÛ

1Raindrop size distribution of different cloud types over the Western Ghats using simultaneous measurements from Micro-Rain Radar and disdrometer

SK DasM Konwar, K Chakravartyc - Atmospheric Research, 2017 - Elsevier

c Elsevier. Atmospheric Research. Volume 186, 1 April 2017, Pages 72-82. Atmospheric Research. Raindrop size distribution of different cloud types over the Western Ghats using simultaneous measurements from Micro-Rain Radar and disdrometer c 3.1. Micro Rain Radar (MRR) c

  Cited by 5 Related articles All 4 versions

y~zƒCƒ“ƒh‚Å‚ÌŠÏ‘ªBMRR‚ð—p‚¢‚Ä~…‚̃^ƒCƒv‚ð”–‚¢‘Η¬«A‘Η¬«A‘wó«A¬‡Œ^‚Ì4‚‚ɕª—ÞB~…‚ÌŠñ—^‚ª‘å‚«‚¢‚Ì‚Í”–‚¢‘Η¬«‚Å‚ ‚Á‚½By—Z‰ð‘w‚ð‘ÎÛ‚Æ‚µ‚Ä‚¢‚È‚¢z

 

[HTML] ametsoc.org

2Intra-event trends in stable isotopes: Exploring midlatitude precipitation using a vertically pointing micro rain radar

CL MullerA BakerIJ Fairchildc - Journal of c, 2015 - journals.ametsoc.org

micro rain radar (MRR) to explore these variations in more detail. MRRs are a relatively new
method of measuring rainfall parameters at a specific location, providing microphysical information
on R, drop size distributions (DSD), fall speed, and height of the 
melting layer [bright c

  Cited by 6 Related articles All 6 versions

y~zƒCƒMƒŠƒX‚Å‚ÌŠÏ‘ªB“¯ˆÊ‘ÌŠÏ‘ª‚Í’·Šú•Ï‰»‚ðŒ©‚éŒ¤‹†‚ª‚Ù‚Æ‚ñ‚Ç‚Å‚ ‚é‚Ì‚Å~‰JƒCƒxƒ“ƒgŠúŠÔ“à‚Ì•ª’PˆÊ‚̕ω»‚𒲂ׂ½B“¯ˆÊ‘̂̕ω»iƒÂDj‚Í~…ƒCƒxƒ“ƒg“à‚Å‚àŒ©‚ç‚êA~…‹­“xA—Z‰ð‘w‚“xA—±Œa‚È‚Ç‚Ì~…“Á«‚É‘å‚«‚­ˆË‘¶‚µ‚½B

 

3Microphysical features of solid/melting particles by Ground-based direct observations for the GPM/DPR algorithm development

K Suzuki, K Nakagawa, Y Kaneko, R Okic - c and Remote Sensing c, 2016 - ieeexplore.ieee.org

c 4). Micro Rain Radar (MRR) was installed with Ka radar at the base of 3942 Page
3. Mt. Zao (215 m ASL). The target of Zao intensive observation was the 
melting layer.
In the early and end of winter, Mt. Zao often has a snowcap c

  Related articlesij

y¢zGPM‚ÌŒŸØB‘ ‰¤ŽRB‰æ‘œ‰ðÍ‚ÌG-PIMMS‚ðŠJ”­‚µ‚½BŽ¼‹…‰·“x1.5‚©‚ç2.1Ž‚ÅoŒ»‚·‚é—Z‰ð•Ï‰»‚ÌŠÏ‘ª‚ɬŒ÷‚µ‚½BiŠÖ˜A˜_•¶G’n㎼‹…‰·“xA‹C‰·Œ¸—¦‚ð‰Á–¡‚µ‚½~…—±Žq‚̃^ƒCƒv‚킯ƒAƒ‹ƒSƒŠƒYƒ€‚̉ü—Ç‚ðŽŽ‚Ý‚½
https://journals.ametsoc.org/doi/abs/10.1175/JHM-D-14-0211.1
j

4Improvement of vertical profiles of raindrop size distribution from micro rain radar using 2D video disdrometer measurements

E Adirosi, L Baldini, N Roberto, P Gatlin, A Tokay - Atmospheric Research, 2016 - Elsevier

c Specifically, installed were a 2D video disdrometer (2DVD) by Joanneum Research mbH, Graz,
Austria (Schönhuber et al., 2007) and a radar vertical profiler termed 
micro rain radar (MRR)
by c In all cases, the 
melting layer was above the highest gate of the MRR. Table 1 c

  Cited by 8 Related articles All 3 versions

y~z‚QDVD‚É‚æ‚é’nã—±Œa•ª•z‚ð—p‚¢‚ÄMRR‚Ì—±Œa•ª•zŠÏ‘ª‚̈—‚ð‰ü‘P‚µ‚½BƒCƒ^ƒŠƒA‚Å‚ÌŠÏ‘ªB

[PDF] nsfc.gov.cn

5c characteristics of raindrop size distributions observed in East China during the Asian summer monsoon season using 2]D video disdrometer and Micro Rain Radar c

L Wen, K Zhao, G ZhangM Xue, B Zhouc - Journal of c, 2016 - Wiley Online Library

c 2265–2282. Research Article Statistical characteristics of raindrop size distributions
observed in East China during the Asian summer monsoon season using 2-D video
disdrometer and 
Micro Rain Radar data. Authors. Long Wen c

  Cited by 7 Related articles All 8 versions

[PDF] nwas.org

y¢z‰Ä‚̃‚ƒ“ƒX[ƒ“‚ð‘ÎÛ‚Æ‚µ‚½“ŒƒVƒi‚Å‚ÌMRR‚Æ2DVD‚Ì“¯ŽžŠÏ‘ªB

~‰J‚ð‘Η¬«‚Æ‘wó«‚É•ª—ÞB‘wó«‚Ì~‰J‚Í•p“x‚ª‘å‚«‚­A‘Η¬«‚Ì~‰J‚Í‘‰J—Ê”ä‚Ö‚ÌŠñ—^‚ª‘å‚«‚¢B‰Ä‚ÌŠúŠÔ‚ð’Ê‚¶‚ÄA—±Œa‚ª¬‚³‚­ŒÂ”‚ª‘å‚«‚¢•ª•z‚̃pƒ^ƒ“‚ªoŒ»‚µ‚Ä‚¢‚½B‚±‚̃pƒ^ƒ“‚̓AƒWƒA‚Ì•Ê‚Ìꊂł͌©‚邱‚Æ‚ª‚Å‚«‚È‚©‚Á‚½B‹ÇŠ“I‚ȃGƒAƒƒ]ƒ‹‚Ì‘‰Á‚ªŒ´ˆö‚Æl‚¦‚ç‚ê‚éB

6 [PDF] Examination of a Winter Storm Using a Micro Rain Radar and AMDAR Aircraft Soundings.

BL Smith, JL Blaes - Journal of Operational Meteorology, 2015 - nwafiles.nwas.org

c This study details how aircraft soundings and a vertically pointing micro rain radar (MRR) were
utilized to monitor changing precipitation types and c in the thermal profile of the environment, and
more specifically, the strength and depth of a warm (
meltinglayer centered around c

  Cited by 3 Related articles All 2 versions 

y¢zƒAƒƒŠƒJ‚Ì“ŒŠCŠÝ‰ˆŠÝ•”‚̓Aƒpƒ‰ƒ`ƒAŽR–¬‚Ì•—‰º‘¤‚É“–‚½‚è—\•ñ‚É‚Í•¡ŽG‚Ì—v‘f‚ª‚©‚ç‚ñ‚Å‚¢‚éB’nŒ`‚ª‹N‚±‚·Š¦‹C‚¾‚Ü‚èicold-air damming[CAD]j‚ÍA~…—±Žq‚̕ω»‚ð•¡ŽG‚ÉA‹}‘¬‚É‚·‚éB2007/1/18‚Ì~…‚ɑ΂µ‚ÄAŒ»‹Æ‚Å‚Í—p‚¢‚ç‚ê‚Ä‚¢‚È‚¢ŠÏ‘ªŽè–@‚ð—p‚¢‚Ä—\‘ª‚µ‚½BŽ–—á‰ðÍ‚É‚æ‚èAq‹ó‹@ŠÏ‘ª‚ÆMRRŠÏ‘ª‚ª‚ǂ̂悤‚É3`6ŽžŠÔæ‚Ì—\‘ª‚ðŒüコ‚¹‚é‚©‚ɂ‚¢‚Äq‚ׂéB‚Ü‚½AMRR‚ÌÚׂȎžŠÔE‹óŠÔ•ª‰ð”\‚É‚æ‚Á‚ĉJAá‚ɕω»‚·‚é—\•ñ‚ª‚æ‚賊m‚É‚È‚Á‚½B

AMDAR: Aircraft Meteorological Data Relay

NWFSO: National Weather Service Forecast Office

 

[PDF] jpier.org

7Performance Evaluation of Micro Rain Radar Over Sumatra Through Comparison with Disdrometer and Wind Profiler

H Hashiguchi, T Shimomai, I Rahayuc - Progress In c, 2016 - jpier.org

c Abstract—Micro Rain Radar (MRR) is a vertical pointing microwave profiler to measure
hydrometeors and related parameters in high resolution c While the 
melting layer height of the two
instruments was the same, the mean Doppler velocities of MRR shown downward increasing c

  Related articles All 4 versions

y~zƒCƒ“ƒhƒlƒVƒAA¼ƒXƒ}ƒgƒ‰“‡‚ÅŠÏ‘ª‚³‚ꂽƒf[ƒ^‚ð—p‚¢‚ÄMRR‚̸“xŒüã‚É‚©‚©‚錤‹†‚ðs‚Á‚½BƒEƒCƒ“ƒhƒvƒƒtƒ@ƒCƒ‰‚ÆParsivel‚Ì“¯ŽžŠÏ‘ª‚ð—˜—p‚µ‚½By—Z‰ð‘w‚ÍŒŸo‚Ì‚Ýz

BLR: 1G‘уEƒCƒ“ƒhƒvƒƒtƒ@ƒCƒ‰

 

[HTML] wiley.com

8[HTML] c associated with vertical air motion in the stratiform region of a springtime rain event from 1290 MHz wind profiler, micro rain radar and Parsivel disdrometer c

DK Kim, DI Lee - Meteorological Applications, 2016 - Wiley Online Library

c Table 2. Specifications of the micro rain radar (MRR). Parameters c 3 Retrieval methodology. In the present study, a spectral method called the Sans Air Motion (SAM) model (Williams 2002)is used to retrieve RSDs and the related rainfall parameters below melting layer c

  Cited by 4 Related articles All 6 versions

y~zŠØ‘B‰ˆŠÝ•”BParsivel‚ƃEƒCƒ“ƒhƒvƒƒtƒ@ƒCƒ‰‚Ì“¯ŽžŠÏ‘ªB—±Œa•ª•z‚ª‘ÎÛB—Ž‰º‘¬“x‚©‚ç—±Œa•ª•z‚ð‹‚ß‚éÛ‚É—Ž‰º‘¬“x‚ðl—¶B

 

 

9Microphysical processes of a stratiform precipitation event over eastern China: analysis using micro rain radar data

H Wang, H Lei, J Yang - Advances in Atmospheric Sciences, 2017 - Springer

c Among the instruments developed that can provide DSD data spatially and continuously, wind
profile radar (WPR) and 
micro rain radar (MRR) are increasingly popular c Huang et al. (2013)
noted that the mean 
melting layer was from 3700 m to 5000 m in Bei- jing, China, from c

  Related articles All 3 versions

y›z’†‘‰ˆŠÝ•”‚Å‚ÌŠÏ‘ªB2mm/hˆÈ‰º‚ÌŽã‚¢~…‚ª‘ÎÛB0.5`1mm‚Ì””Z“x‚Í—Z‰ð‘w‚æ‚艺‚Å‚Ù‚Æ‚ñ‚Ǖω»‚µ‚È‚©‚Á‚½BÅ‘å‚̃hƒbƒvƒ‰‘¬“xA‚¨‚æ‚уhƒbƒvƒ‰‘¬“x‚ÌÅ‘å•Ï‰»‚Í—Z‰ð‘w‚Ì’¼‰º‚ÅŠÏ‘ª‚³‚ꂽB‚»‚±‚Ńhƒbƒvƒ‰‘¬“x‚Æ‘¬“x•Ï‰»‚ð—p‚¢‚Ä—Z‰ð‘w‚Ì‚“x‚ÆŒú‚³‚ð’è‹`‚·‚é•û–@‚ðŠm—§‚µ‚½B~á—±Žq‚Ì—Ž‰º‘¬“x‚Í—Z‰ð‘w‚æ‚èã‚Å‚Ì—±Žq”»•Ê‚É—p‚¢‚邱‚Æ‚ª‚Å‚«‚éB’Šo‚µ‚½~…ƒCƒxƒ“ƒg‚Ìʼn‚Ì20•ª‚Í—Z‰ð‘w‚æ‚èã‚ÅèÅ‚ª‘ì‰z‚µ‚Ä‚¢‚½B‚“x2000m‚Å‚ÍèÅ‚ªÅ‰‚Ì250•ª‚É‚æ‚­Œ©‚ç‚ꂽB‚»‚Ì‚ ‚Æ‚Ì150•ª‚Í—Z‰ð‘w‚Ìã‚ÅèÅ‚Æ…“H‚𔺂Á‚½˜Z‰Ô‚ª„’肳‚ꂽB

y—v’²¸z~…Ží‚Ì”»’è‚É—p‚¢‚½‘ªŠí

2017 Hong Wang, Hengchi Lei @Advances in Atmospheric Sciences  pp 1472–1482

 

[HTML] tandfonline.com

10An observational study on vertical raindrop size distributions during stratiform rain in a semiarid plateau climate zone

Y Chen, JL An, HZ Liu, J Duan - Atmospheric and Oceanic Science c, 2016 - Taylor & Francis

c Vertical raindrop size distributions of two stratiform rain events were measured with a Micro Rain Radar during summer 2009 at a semiarid continental c rate, total raindrop numbers, and parameters (a and b) of the Z–R relationship was small below a melting layer, suggesting that c

  Related articles All 4 versions

y~z’†‘‚ÌŠ£‘‡’n‹æiXilinhot, China (4338ŒN, 11642ŒE)j‚Å2‚‚̑wó«~…‚ðŠÏ‘ªBsequential intensity filtering technique (SIFT)‚È‚éƒtƒBƒ‹ƒ^ƒŠƒ“ƒO‚É‚æ‚Á‚ÄZRŠÖŒWŽ®‚ÌŒW”‚ª‚æ‚­‡‚¤‚悤‚É‚È‚éi~…—Ê„’è‚̂΂ç‚‚«‚ª¬‚³‚­‚È‚éjB‰”’¼•ûŒü‚̕ω»‚Å‚Í—Z‰ð‘w‚æ‚艺‚Å•Ï“®‚ª¬‚³‚¢B“–ŠY—̈æ‚Å‚ÍZR–@‚É‚æ‚é~‰J„’肪—LŒøB

 

Page2

[PDF] tuat.ac.jp

1Convective rain study with radiometer, radar and electric field observations at a tropical location

A MaitraS Jana, R Chaktaborty - Antennas and Propagation c, 2016 - ieeexplore.ieee.org

c radiometer measures brightness temperatures at 14 frequencies at two frequency bands, namely, 22.24-31.4 GHz and 51.3-59 GHz [5]. A micro rain radar (MRR) is used to classify the rain as convective or stratiform based on the melting layer signature in the rain rate profile c

  Related articles All 4 versions

y~zƒJƒ‹ƒJƒbƒ^iŠCŠÝ‚Æ—¤‚ªÚ‹ß‚µ‚Ä‚¢‚éêŠj‚Å‘½”g’·ƒ}ƒCƒNƒ”g•úŽËŒvAMRR‚Æ‚Ì“¯ŽžŠÏ‘ªB~…—ʂ̉”’¼•ª•zA‰_…—ÊA—±Œa•ª•zA“dê‚Ì•Ï“®‚ð•]‰¿B·‚µ”—‚Á‚½~…‚ð—\‘ª‚·‚邽‚ß‚É‘½”g’·‚Ì‹P“x‰·“x‚ðŠˆ—p‚µ‚½B‘Η¬«‚Ì~…‚ªŽn‚Ü‚é‘O‚Í31.4G‚Ì‹P“x‰·“x‚ª‚‚­‚È‚è“dê‚Ì•Ï“®‚ª‘å‚«‚­‚È‚Á‚½B

 

2Vertical profile of rain: Ka band radar observations at tropical locations

S DasA Maitra - Journal of Hydrology, 2016 - Elsevier

c Moreover, the variation of VPR near ground (<1 km) and above up to the melting layer is usually assumed to be similar which may c In this paper, we report some statistical observations of vertical rain structure obtained using a vertical looking Micro Rain Radar(MRR) in Ka band c

  Cited by 5 Related articles All 3 versions

y¢z”M‘шæ3‰ÓŠ‚ÅMRR‚É‚æ‚éŠÏ‘ª‚ðŽÀŽ{‚µ‚½B~…‹­“x‚ª2mm/h‚æ‚謂³‚¢‚Æ—±Œa•ª•z‚É‚¨‚¢‚Ĭ—±Žq‚ª‘ì‰z‚·‚éB20mm/h‚ð’´‚¦‚é‚Æ~…‹­“x‚Æ‚Æ‚à‚É—±Œa‚à‘å‚«‚­‚È‚éB

 

 

[PDF] ursi2016.org

3Dependence of rain integral parameters on measured rain drop velocities at a tropical location

T SarkarS JanaA Maitra - URSI Asia-Pacific Radio Science c, 2016 - ieeexplore.ieee.org

Micro rain radar Micro rain radar (MRR) is a vertically pointing frequency modulated
continuous wave radar (FM-CW) radar c The presence of 
melting layer can be identified
by observing the bright band signature in radar reflectivity profile c

  Related articles All 3 versions

y¢za Laser Precipitation Monitor (LPM) ƒJƒ‹ƒJƒbƒ^‚Å‚ÌŠÏ‘ªB‘å—±Žq‚ÅAI’[‘¬“x‚æ‚葬‚¢—±ŽqA‚ä‚Á‚­‚è‚Æ—Ž‰º‚·‚é—±Žq‚ª‘¶Ý‚·‚éB‚»‚Ì”‚͑Η¬«‚æ‚è‚à‘wó«‚Å‘½‚¢B‘Η¬«‚Æ‘wó«‚É•ª‚¯‚ÄZRŠÖŒWAARŠÖŒW‚𒲸B

 

4Effects of melting layer on Ku-band signal depolarization

T SarkarS DasA Maitra - Journal of Atmospheric and Solar-Terrestrial c, 2014 - Elsevier

c band satellite signal in the presence of melting layer has been investigated with the experimental data at Kolkata (22‹34ŒN, 88‹29ŒE), India. 2. Experimental details. For our present study we have used the data from an impact type Disdrometer, a Micro Rain Radar (MRR) and c

  Cited by 12 Related articles All 3 versions

y¢zƒCƒ“ƒhKolkata‚Å‚ÌŠÏ‘ªBÃŽ~‰q¯NSS6‚É‚æ‚éKu‘Ñ‚Ì“`”ÀŒvŽZ‚ÌŒ¤‹†Bƒuƒ‰ƒCƒgƒoƒ“ƒh“à‚ð“d”g‚ª’ʉ߂·‚éÛ‚É•½sico-polarj¬•ª‚ÌŒ¸Š‚Æ’¼Œð¬•ª‚Ì‹­‰»‚ɂ‚¢‚Ä’²‚ׂ½B’nã—±Œa•ª•z‚ÍA‘wó«‚̉J‚Ŭ‚³‚¢—±Žq‚ª‘½‚­‘Η¬«‚̉J‚Å‘å—±Žq‚ðŒ`¬‚µ‚Ä‚¢‚½BŠÏ‘ªŒ‹‰Ê‚©‚ç—±Žq—Z‰ð‚É‚æ‚é…•½‰”’¼•Î”g‚Ì‹­“x·‚ÍAŽã‚¢~…‚Å‚Ì—±Žq•ª—ô‚̉ߒöy—±Žq‚ªG•½‚É‚È‚éŒø‰Êz‚æ‚èŒø‰Ê‚ª‘å‚«‚©‚Á‚½ByŠÏ‘ª‚ÉARD80,MRR‚ð—˜—pz

 

5Simultaneous radar observations of vertical profile of rain features from space and ground at Ku and Ka bands at a tropical location

G RakshitA Maitra - Mapan, 2016 - Springer

c CrossRefGoogle Scholar. [20]. PK Kunhikrishnan, BR Sivaraman, NK Kumar and DP Alappattu,
Rain observations with 
micro rain radar (MRR) over c 996–1012.ADSCrossRefGoogle Scholar.[22]. W. Klaassen, Radar observations and simulation of the melting layer of precipitation c

  Cited by 3 Related articles

y¢zy—v’²¸z‰q¯ŠÏ‘ª‚ÆMRR‚ð‘g‚݇‚킹‚Ä~…‚Ì“Á«‚𒲸B“ñ”g’·ƒŒ[ƒ_‚ð—˜—pB‰q¯ŠÏ‘ªƒf[ƒ^‚Æ’nã~…‚̉”’¼ƒvƒƒtƒ@ƒCƒ‹‚ð‘g‚݇‚킹‚éŒø‰Ê‚ðŽ¦‚·B

 

6The Chilean Coastal Orographic Precipitation Experiment: Observing the Influence of Microphysical Rain Regimes on Coastal Orographic Precipitation

AK Massmann, JR Minderc - Journal of c, 2017 - journals.ametsoc.org

  Cited by 1 Related articles All 4 versions

y›zƒ`ƒŠ‚ÌNahuelbutaŽRi1.3kmj‚Å’g‚©‚¢‰_‚̉ߒö‚Æ•X»‰ß’ö‚Ì“Á’¥‚ð‰ð–¾‚µAŽRŠxˆæ‚Å‚»‚ꂼ‚ê‚̉ߒö‚ª‚ǂ̂悤‚ɘA‘±‚µ‚Ä‚¢‚é‚©‚𒲂ׂ½B‚Ó‚à‚Æ‚Å‚Í23“‚ª’g‚©‚¢‰_‚̉ߒöA50“‚ª•X»‰ß’ö‚©‚ç”­¶‚µ‚Ä‚¢‚½BŽRŠx‚ÌŒø‰Ê‚ð‚Ù‚Ú“¯ˆÜ“x‚̃JƒŠƒtƒHƒ‹ƒjƒA‚Æ”äŠr‚µ‚Ä‚Ý‚½B’nŒ`‚É‚æ‚éŒø‰Ê‚Í—¼‰ß’ö‚Å‚‚­Aã‹ó‚©‚ç‚̃V[ƒfƒBƒ“ƒO‚ÍŽRŠxŒø‰Ê‚Ì‚½‚ß‚É•K‚¸‚µ‚à•K—v‚Å‚È‚¢‚ÆŽ¦´‚³‚ꂽyŽR‚ª’á‚¢iHjƒJƒŠƒtƒHƒ‹ƒjƒA‚Å‚à‘å‚«‚È’nŒ`Œø‰Ê‚ª”­¶‚µ‚Ä‚¨‚èA’nŒ`Œø‰Ê‚Íã‹ó‚©‚ç‚ÌŽí‚Ü‚«‚̉e‹¿‚Å‚È‚¢‚ÆŽv‚í‚ê‚ézBŠÏ‘ª‚©‚ç’nŒ`Œø‰Ê‚Í’g‚©‚¢‰_‚ւ̉e‹¿‚Ì‚Ù‚¤‚ª‘å‚«‚¢‚ªA’nŒ`Œø‰Ê‚Í•X»‚Ì‚ ‚é‚È‚µ‚É‚©‚©‚í‚ç‚È‚¢Bƒ]ƒ“ƒfŠÏ‘ª‚É‚æ‚é‰ðÍ‚Å‚ÍA‰º‘w‚Ì…ö‹Cƒtƒ‰ƒbƒNƒXA–³ŽŸŒ³‰»‚µ‚½•W‚‚É‚æ‚éˆá‚¢‚Å‚ÍA—¼‰ß’ö‚Ì’nŒ`Œø‰Ê‚̈Ⴂ‚ðà–¾‚Å‚«‚È‚©‚Á‚½B

 

[PDF] academia.edu

7Assessment of different raindrop size measuring techniques: Inter-comparison of Doppler radar, impact and optical disdrometer

T SarkarS DasA Maitra - Atmospheric Research, 2015 - Elsevier

Micro rain radar (MRR) is a vertically pointing FM-CW radar that measures the evolution of DSD spectra and drop velocity of rain above ground c Radar reflectivity profile indicates the presence of melting layer by a radar bright band signature (Das et al., 2010; Peters et al., 2002 c

  Cited by 11 Related articles All 5 versions

y~‹@Ší‚Ì”äŠrzMRR‚ÆŒõŠw“IAƒCƒ“ƒpƒNƒgŽ®ƒfƒBƒXƒhƒƒ[ƒ^‚Ì”äŠrB‘å—±ŒaA¬—±Œa‚ÌŠ´“x‚Í‚Ç‚Ì‘ªŠí‚à‚æ‚­‚È‚¢B

 

8Seasonal variation of DSD parameters during stratiform and transitional precipitation over a coastal station Thumba (8.5‹ N, 76.9‹ E)

NVPK Kumar, S Lavanya - Remote Sensing of the Atmosphere c, 2016 - spiedigitallibrary.org

c hydrometeors also shows a gradient around the melting layer with narrow and wide distributions above and below the melting layer, respectively c DSD) and other microphysical parameters in the altitude region of 200m – 3.6 km are derived using the Micro rain Radar at Thumba c

  Related articles All 4 versions

y¢—±Œa•ª•z‚Ì‚“x•Ï‰»zMRR‚É‚æ‚é—±Œa•ª•z•]‰¿‚ð‘wó«A‘JˆÚŒ^‚ɂ‚¢‚Ä’²‚ׂ½B—±Œa•ª•z‚Ì‚“x•Ê•p“x•ª•z‚ð쬂µ‚½Bö”­EÕ“ËE•¹‡‚Æ‚¢‚Á‚½”÷•¨—‰ß’ö‚𒲂ׂé‚Ì‚ÉMRR‚Í—LŒøB

 

[HTML] ametsoc.org

9Radar observation of evaporation and implications for quantitative precipitation and cooling rate estimation

X Xie, R Evaristo, S Troemelc - c of Atmospheric and c, 2016 - journals.ametsoc.org

c The motivation of this study, which relates observations of a vertically pointing K-band Micro Rain Radar(MRR) and a polarimetric X-band c with an analysis of the sensitivity of polarimetric variables and surface precipitation to initial DSDs below the bottom of the melting layer c

  Cited by 5 Related articles All 3 versions

y¢—Z‰ð‘w‚æ‚艺‚Ì—±Žq•Ï‰»z~…‚Ìö”­Œø‰Ê‚ðƒŒ[ƒ_‚©‚焒肵A’nã~…‚ւ̉e‹¿‚𒲂ׂéBö”­‚É‚æ‚Á‚ÄZ‚ͬ‚³‚­ZDR‚Í‘å‚«‚­‚È‚éB¬—±Žq‚ªæ‚É‚È‚­‚È‚é‚Ì‚ÅBã‹ó‚Æ’nã‚ÌŠÏ‘ª‚̈Ⴂ‚ð‰ðŽß‚·‚邱‚Æ‚É‚æ‚è~…ŠÏ‘ª‚̸“x‚ðŒüã‚·‚éBMRR‚ÍBB”»’è‚É—˜—pB

 

10Impacts of orography and rain intensity on rainfall structure. The case of the HyMeX IOP7a event

J Zwiebel, J Van Baelen, S Anquetinc - Quarterly Journal of c, 2016 - Wiley Online Library

c Houze (2003a) presented a conceptual model of the air-flow and microphysics of the orographic precipitation mechanism in which growth processes of droplets are enhanced by the local topography through riming (above 0 ‹C) and through coalescence below the melting layer c

  Cited by 8 Related articles All 2 versions

y¢ŽRŠx’n‚Ì~…—±Žq•Ï‰»zƒtƒ‰ƒ“ƒX‚Å‚ÌW’†ŠÏ‘ª‚ÌŒ‹‰ÊBŽRŠxˆæ‚Å‚Í•¹‡‰ß’ö‚¨‚æ‚Ñ—±Žq‚Ìö”­‚ªd—v‚Å‚ ‚邱‚Æ‚ª‚í‚©‚Á‚½BLWC‚ª‘½‚¢‚ÆÕ“Ë‚ª‹­‰»‚³‚ê‚éBy—vŽ|‚ÉMRR‚È‚µz

 

Page3|~FŒ¸Š•â³‚È‚Çi—Z‰ð‘w‚ð‘ÎÛ‚É‚µ‚Ä‚¢‚È‚¢jA¢F~…Œ`¬‰ß’ö‚ðˆµ‚¤

1Rain microphysical features as observed from ground based radar and disdrometer at a tropical location

S Majumder, A Adhikari, A Maitra - Computers and Devices for c, 2015 - ieeexplore.ieee.org

c time of 30 second [9]. Another instrument which has been used for the present work is a vertically pointing Micro Rain Radar (MRR) collocated c Bright band indicates the presence of melting layer in startiform events [1, 9]. We have classified the rain events during 2012- 2013 into c

  Related articles

y~MRR‚ð—p‚¢‚½~…ƒ^ƒCƒv‚Ì•ª—Þz

 

[PDF] researchgate.net

2Effect of vertical wind on rain drop size distributions in the boundary layer

G RakshitR Chakrabortyc - Antennas and Propagation c, 2016 - ieeexplore.ieee.org

c Fig. 4. Vertical wind profile 4. Conclusions The evolution of drop size distribution at different
heights has been studied from 
micro rain radar observations during convective rain events at
a tropical location c "Effects of 
melting layer on Ku-band signal depolarization," J. Atmos c

  Cited by 2 Related articles All 3 versions

y¢—Z‰ð‘w‚æ‚艺‚Ì—±Œa•ª•z•Ï‰»zBB’¼‰º‚ÌZ‚̋ɬ‚Í—±Žq‚Ì•ª—ô‚É‚æ‚é‚Æl‚¦‚ç‚ê‚é

 

[HTML] sciencedirect.com

3[HTML] Estimating the snowfall limit in alpine and pre-alpine valleys: A local evaluation of operational approaches

M Fehlmann, E Gascón, M Rohrer, M Schwarbc - Atmospheric c, 2018 - Elsevier

c Keywords. Snowfall limit; Melting layer; Precipitation type; Early warning; Micro rain radar; Bright band. 1. Introduction. The snowfall limit has important implications for different hazardous processes associated with prolonged or heavy precipitation c

  All 2 versions

y¢áü—\•ñ‚Ì‚“x‰»BMRR‚ð—p‚¢‚Ä—\•ñ‚ð•â³‚·‚éz—\‘ªæsŽžŠÔ‚ª6ŽžŠÔ’ö“x‚ð‘ÎÛB”“ú‚Ì—\•ñ‚ɂ‚¢‚Ă̓Aƒ“ƒTƒ“ƒuƒ‹‚ð—˜—pB—Zá—¬o‚É—˜—pB

 

[HTML] ametsoc.org

4The midlatitude continental convective clouds experiment (MC3E)

MP Jensen, WA Petersen, A Bansemerc - Bulletin of the c, 2016 - journals.ametsoc.org

  Cited by 36 Related articles All 13 versions

y~zƒAƒƒŠƒJ‚Å[‚¢‘Η¬‚ð‘ÎÛ‚Æ‚µ‚½W’†ŠÏ‘ª‚ÌЉîB

 

[PDF] researchgate.net

5Evaluation of Operational and Experimental Precipitation Algorithms and Microphysical Insights during IPHEx

JM ErlingisJJ GourleyPE Kirstetterc - Journal of c, 2018 - journals.ametsoc.org

c 2015). Wilson and Barros (2014) relate the increase of reflectivity toward the ground in Micro
Rain Radar observations with the interactions between low-level clouds and fog and precipitation,
as well as model moisture convergence patterns required to produce the low-level c

  Related articles All 3 versions

y¢ŽRŠx‚ª~…Œ`¬‰ß’ö‚É—^‚¦‚é‰e‹¿‚𒲸zX‘уŒ[ƒ_‚ð—˜—pBŽR’n‚Ì•—㑤‚Å‚Í•¹‡‰ß’ö‚ª‘ì‰zB’J•”‚Å‚Í•¡‡‰ß’ö‚ª‹N‚«‚Ä‚¢‚éB’nŒ`‚É‚æ‚é‹­§ã¸‚ª‘Η¬‚ðˆÛŽ‚µA’†‰›—±Œa‚Ì‘å‚«‚È~…—±Œa•ª•z‚Æ‚È‚éB

 

6Estimation of the liquid water content and Z–LWC relationship using Ka]band cloud radar and a microwave radiometer

SB Oh, YH Lee, JH Jeong, YH Kimc - Meteorological applications c, 2018 - Wiley Online Library

c Figure 8. Flowchart of classification processing for echo types using micro rain radar rain rate
(MRR RR) and ceilometer cloud base height (Ceil c First, to avoid the effects of ice cloud droplets,
echoes that were below the 
melting layer were used to derive Z–LWC rela- tionships c

  Related articles

y~LWC‚Ì3ŽŸŒ³•ª•zì¬‚ðŽŽ‚Ý‚½z‰_ƒŒ[ƒ_‚ð—p‚¢‚ÄZ-LWCŠÖŒW‚ðì¬BZ-LWCŠÖŒW‚͉_‚̃^ƒCƒv‚É‚æ‚Á‚ĈقȂèA‰_ƒŒ[ƒ_iKaCRj‚̃GƒR[‚ðu”ñ~…‰_vu~…‰_v‚¨‚æ‚ÑMRR‚Å”»’f‚µ‚½u—±Œa•ª•zv‚Å•ª—Þ‚µA‚»‚ꂼ‚ê‚ɂ‚¢‚ÄZ-LWCŠÖŒW‚ð‹‚ß‚½B

 

[HTML] ametsoc.org

7Precipitation and cloud structures of intense rain during the 2013 Great Colorado Flood

K FriedrichEA Kalina, J Aikinsc - Journal of c, 2016 - journals.ametsoc.org

c resulted in surface convergence. During times of weak forcing, shallow convection produced rain at and below the melting layer through collision–coalescence and, to a lesser extent, riming. A mesoscale circulation interacting c

  Cited by 12 Related articles All 4 versions

y¢‘å^…‚ð‚à‚½‚炵‚½‰_‚̉ðÍBŽÎ–Ê㸂ɂæ‚镹‡‰ß’ö‚ÌŒø‰Ê‚ðŽw“EzMRR‚Í—Z‰ð‘w‚æ‚èã‚ÅŒ¸Š‚̉e‹¿‚ª‘å‚«‚¢‚Ì‚ÅAƒhƒbƒvƒ‰‘¬“x‚Ì‚Ý‚ð—p‚¢‚éB

 

[PDF] academia.edu

8Multi-technique observations of convective rain events at a tropical location

A MaitraS JanaR Chakrabortyc - General Assembly and c, 2014 - ieeexplore.ieee.org

c For the present study we have used the data from an EFM, an impact type disdrometer, a micro rain radar (MRR) and a multi frequency radiometer located at the Institute of c Thus it is capable of indicating the presence of melting layer by bright band signatures during rain events c

  Cited by 14 Related articles All 5 versions

y~‘å‹C‚Ì“dêŠÏ‘ªzMRR‚Í‘wó«A‘Η¬«‚Ì•ª—Þ‚É—˜—p

 

[HTML] ametsoc.org

9Global Precipitation Measurement Cold Season Precipitation Experiment (GCPEX): For measurement's sake, let it snow

G Skofronick-Jackson, D Hudakc - Bulletin of the c, 2015 - journals.ametsoc.org

  Cited by 17 Related articles All 8 versions

y~GPM“~ŠúƒLƒƒƒ“ƒy[ƒ“‚Ìà–¾zá‚Ì”÷•¨—“I“Á’¥‚𒲸‚·‚邱‚Æ‚ª–Ú“IB

ŠÖ˜A˜_•¶Fhttps://link.springer.com/article/10.1007%2Fs00703-011-0142-z

MRR‚ð—p‚¢‚½‰_ƒŒ[ƒ_‚ÌŒŸØ

ŠÖ˜A˜_•¶Fhttp://onlinelibrary.wiley.com/doi/10.1029/2011JD016579/abstract

MRR‚Æ•úŽËŒv‚Ì”äŠr

[PDF] environmentanalytics.com

10Characteristics of Precipitating Storms in Glacierized Tropical Andean Cordilleras of Peru and Bolivia

LB Perry, A Seimon, MF Andrade-Floresc - Annals of the c, 2017 - Taylor & Francis

c new high-elevation comprehensive precipitation monitoring stations at Chacaltaya, Bolivia, and
the Quelccaya Ice Cap, Peru; and a vertically pointing 
Micro Rain Radar—this article c (2) What
is the vertical structure (eg, reflectivity, Doppler velocity, 
melting layer heights) of c

  Cited by 2 Related articles All 2 versions

y¢ƒAƒ“ƒfƒXŽR–¬‚Å‚Ì~…‚Ì“Á’¥‚̉ðÍzMRR‚Í~…‚̉”’¼•ª•zA—Z‰ð‘w‚“x‚𒲸‚·‚邽‚ß‚É—˜—pB

 

Page4

1Rain attenuation over earth space path from radar and propagation measurements at tropical location

BK GuhaR Chakraborty, B Nandyc - c and Devices for c, 2015 - ieeexplore.ieee.org

Micro Rain Radar (MRR), which is an FM-CW Radar at 24GHz, has been utilized to obtain drop size distribution and the vertical rain rate c also signifies the presence of high specific attenuation in the height range of 5 km probably due to the presence of melting layer structure in c

  Cited by 2 Related articles All 3 versions

y~Œ¸Š•â³‚ɂ‚¢‚Ä‚Ì’²¸zƒCƒ“ƒhAƒJƒ‹ƒJƒbƒ^B

 

2Precipitation Observations with NSSL's X-band Polarimetric Radar during the SNOW-V10 Campaign

TJ Schuur, AV Ryzhkov, DE Forsyth, P Zhangc - Pure and Applied c, 2014 - Springer

c partial beam blockage is eliminated in the R(A) field. 4 Evolution of the Radar-derived
Melting Layer on 30–31 January 2010 and Comparisons with Micro Rain Radar
Measurements. For ranges within 30 km, the NO-XP radar is c

  Cited by 7 Related articles All 7 versions

y›z‰Â”ÀŒ^‚ÌXƒoƒ“ƒhMPƒŒ[ƒ_‚ð—p‚¢‚ÄAƒoƒ“ƒN[ƒo[ŒÜ—ւ̃iƒEƒLƒƒƒXƒg¸“x‚ðŒüãBMPŠÏ‘ª‚É‚æ‚Á‚Ä—Z‰ð‘w‚“x‚̕ω»‚ðÚׂɒ²‚ׂ½B‚“x•Ï‰»‚ÍMRR‚ƈê’v‚µ‚½BMPŠÏ‘ª‚©‚ç‚í‚©‚é“Á’¥‚Æ‚µ‚Ä‚ÍA’nã•t‹ß‚ÅZDR‚ª‹­‰»‚³‚ꂽB—±Œa‚É‚æ‚é—Ž‰º‘¬“x‚̈ႢA‚ ‚é‚¢‚ͬ—±Žq‚ª—Dæ“I‚Éö”­‚·‚邱‚Æ‚É‚æ‚éB—Z‰ð‘w‚æ‚èã‚Å‚ÍA‚Z’áZDR‚ƒÏHVˆæ‚ł͑Η¬‚É‚æ‚è‹ÃW‚Ü‚½‚ÍA‰_—±•t’…‚ª‘ì‰z‚µ‚Ä‚¢‚é‚Æl‚¦‚ç‚ê‚éB‚³‚ç‚Éã‹ó‚Å‚ÍZDR‚ª‘å‚«‚¢—̈悪‚ ‚è‹}‘¬‚ȘZ‰Ô‚̬’·‚Æ‹ÃW¬’·‚ÌŠJŽn‚ðŽ¦´‚·‚éB‚±‚Ì“Á’¥‚ÍS‘ÑAC‘т̃Œ[ƒ_‚Å‚àŠÏ‘ª‚³‚ꂽB

y—v’²¸FMRR‚Ì–ðŠ„z

 

[PDF] rero.ch

3Estimation of snowfall limit for the Kashmir Valley, Indian Himalayas, with TRMM PR Bright Band information

S Schauwecker, M Rohrer, M Schwarbc - Meteorologische c, 2016 - doc.rero.ch

c that the height of the BB ob- served by TRMM and a ground-based vertically looking Micro Rain
Radar are in good agreement. They further- more suggest that TRMM 3A25 5 ~ 5 degree grid
data can be a good information source for average 
melting layer characteristics where c

  Cited by 3 Related articles All 5 versions

BB‚Ì‹CŒó’l‚ðáü‚Ì”»’f‚É—˜—pzTRMM-PR‚ð—p‚¢‚½BB‚Ì”»’èB‚•W‚•”‚Å‚ÌŠÏ‘ª‚ð—p‚¢‚ÄŒŸØB

 

4Polarimetric Radar Observation of Evaporation and the Implications for Rainfall Precipitation Estimation

P Saavedra, X Xie, C Simmer - AGU Fall Meeting Abstracts, 2015 - adsabs.harvard.edu

c Two cases of evaporation processes observed by a polarimetric radar and micro rain radar are
shown to offer a detail insight into the evaporation process and the related DSD evolution. The
first event where an initial Zdr below the 
melting layer is observed above 1.5 dB c

 

y¢zö”­‚ÌŒø‰Ê‚ª—±Œa•ª•z‚É—^‚¦‚é‰e‹¿‚𒲸B—Z‰ð‘w‚æ‚艺‚ª‘ÎÛB

 

5How does nature of rain affect micro-physical parameters of surface rain? A study on vertical profile and surface rain micro-structure over eastern Himalaya in India

S Singh, A Chatterjee, S Ghoshc - 40th COSPAR c, 2014 - adsabs.harvard.edu

c A vertical looking Micro Rain Radar (MRR) was used for the vertical profile of
micro-physical parameters of rain along with the rain height derived from the bright
band structure of 
melting layer of radar reflectivity profile. The c

 

y¢‰_ƒ^ƒCƒv–ˆ‚Ì—±Œa•ª•zzƒqƒ}ƒ‰ƒ„‚Å‚ÌŠÏ‘ªi•W‚2,200mj‚Å‚ÌŠÏ‘ªB‘Η¬«‚̉_‚Å‚ÍŽž‚É100mm¥h‚É’B‚µ‘å—±Žq‚ª5mm‚ð’´‚¦‚éB

 

[PDF] researchgate.net

6Observations of vertical rain structure using space borne and ground based radars at a Tropical location

G RakshitA Maitra - Computers and Devices for c, 2015 - ieeexplore.ieee.org

c The measuring principle of the micro rain radar is based on the Doppler effect of radio signal
of frequency of 24 GHz, which observes the rain parameters such as radar c In general it is observed
that the 
melting layer is well identified by both the instruments at similar heights c

  Related articles All 2 versions

y~MRR‚ÆTRMM‚Ì”äŠrzƒJƒ‹ƒJƒbƒ^

 

[PDF] washington.edu

7Stratiform precipitation processes in cyclones passing over a coastal mountain range

JP Zagrodnik, LA McMurdiec - Journal of the c, 2018 - journals.ametsoc.org

c coast to middle elevations. At the latitude of OLYMPEX, the melting layer in storms
arriving 78 from c (2017), a vertically 265 pointing 
Micro Rain Radar (MRR) at the Fishery site indicated non-bright band rain by their 266 criteria c

  Cited by 1 Related articles

y¢•—Œü‚ªŽÎ–ÊŒü‚«‚Ìꇂͬ—±Žq‚ªŒ`¬‚³‚ê~…‚ª‹­‰»‚³‚ê‚éBŽÎ–Ê‚É•ÀsA‚Ü‚½‚ÍAŽÎ–Ê‚ð‰º‚éŒü‚«‚Ìꇂͬ—±Žq‚ªö”­‚ÅŽæ‚蜂©‚ê‚é‚Ì‚Å~…‚Í‚ ‚Ü‚è‹­‚­‚È‚ç‚È‚¢zŠCŠÝü‚©‚ç‚Ì‹——£‚Æ•W‚‚̈Ⴂ‚É‚æ‚é—±Œa‚̈Ⴂ‚ɂ‚¢‚ÄB‹­‰J‚͉º‘w‚Ì’nŒ`‚É‚æ‚Á‚Ä“Á’¥•t‚¯‚ç‚ê‚éB¬‚©‚ç’†—±ŽqA‚¨‚æ‚ÑA‘å—±Žq‚ð‘‚â‚·By—v’²¸G‹­‰J‚ª‘ÎÛ‚È‚Ì‚ÅMRR‚Ì—˜—p‚ÍŒÀ’è“IB‚¨‚»‚ç‚­ƒuƒ‰ƒCƒgƒoƒ“ƒhŒŸoiNBB~…‚Ì’Šoj‚É—˜—pz

 

8Monitoring the absolute calibration of a polarimetric weather radar

M Frech, M Hagen, T Mammen - Journal of Atmospheric and c, 2017 - journals.ametsoc.org

c This is verified usingMicro Rain Radar (MRR) c To verify this conclusion, we have installed
a vertically looking 
Micro Rain Radar (MRR; Peters et al. 2005) that is able to fill the gap between
the far field of the operational C-band radar and the disdrometer c

  Cited by 5 Related articles All 4 versions

[HTML] ametsoc.org

y¢zƒŒ[ƒ_‚ÅŠÏ‘ª‚·‚éZ‚Æ’nã‚ÌZ‚ð1dBˆÈ“à‚ňê’v‚³‚¹‚鎎‚ÝB200m‚Í‚È‚ê‚ÄÝ’u‚µ‚½‰J“HŒv‚É‚æ‚è’nãŠÏ‘ª‚Ì‘ã•\§‚ð•]‰¿BMRR‚Íã‹ó‚Æ’nã‚ÌŠÏ‘ª‚𖄂߂邽‚ß‚É—˜—pB

 

9Evidence for a Nimbostratus Uncinus in a Convectively Generated Mixed-Phase Stratiform Cloud Shield

JM Schmidt, PJ Flatauc - Journal of the Atmospheric c, 2017 - journals.ametsoc.org

c average of the two abovementioned ice and liquid water content relations across the melting-layer depth. The final velocity and derived ice–liquid water content estimates were compared against those derived independently from the Metek K-band Micro Rain Radar (MRR) c

  Related articles

y¢z—‘w‰_‚Ì’†‚Ì”gó‰_(billow cloud)‚ð50‡p‚Ì•ª‰ð”\‚ðŽ‚‰”’¼ƒŒ[ƒ_‚Å’²‚ׂ½B—‘w‰_‚Ì’†‚ÉŽüŠú“I‚ȕω»‚ªŒ©‚ç‚ꂽB‚l‚q‚q‚Í•½‹Ï\‘¢‚ÌŠm”F—pB

 

[PDF] rero.ch

10The freezing level in the tropical Andes, Peru: an indicator for present and future glacier extents

S Schauwecker, M Rohrer, C Huggelc - Journal of c, 2017 - Wiley Online Library

c data from two climate reanalysis products, Tropical Rainfall Measuring Mission (TRMM)
Precipitation Radar Bright Band data, 
Micro Rain Radar data, and c mass balance and runoff for
tropical glaciers The SLH is defined as the top of the 
melting layer during precipitation events c

  Cited by 5 Related articles All 7 versions

y~zƒyƒ‹[‚Ì•X‰Í‚̬’·EÁŽ¸‚𒲂ׂ邽‚ß‚É‚s‚q‚l‚l‘¼‚Ì‘ªŠí‚ð—p‚¢‚Ä0Ž‚“x‚̕ω»‚ðŒŸØ‚µ‚½B

 

Page5

1Anomalies in relative humidity profile in the boundary layer during convective rain

R ChakrabortyS TalukdarU SahaS Janac - Atmospheric Research, 2017 - Elsevier

c Liquid water content profiles for the study have been taken from Micro Rain Radar
(MRR) observations. MRR c heights. Thus, it is capable of indicating the presence
of 
melting layer by bright band signatures during rain events c

  Cited by 6 Related articles All 6 versions

y~z‘Η¬«‚Ì~…’†‚ÉŒ©‚ç‚ê‚éA‘Š‘ÎŽ¼“x‚̋ɬ•”‚ɂ‚¢‚ÄBŒ¸—¦‚ª’á‚­‚È‚èAö”M‚ª‚‚¢‚Æ‚±‚ë‚Å”­¶‚·‚éy㉺‚æ‚è’g‚©‚¢‚Æ‚±‚ë‚Å‚Í‘Š‘ÎŽ¼“x‚ͬ‚³‚­‚È‚ézB‘wó«‚̉_‚Å‚Í”­¶‚µ‚È‚¢B

 

2Rainfall observations and assessment using vertically pointing radar and X-band radar

N Mazari, HO SharifH Xie, AE Tekelic - Journal of c, 2017 - jh.iwaponline.com

Skip to main content. Main menu. About the Journal: Aims & Scope; Editorial Board;
Browse Archive; Abstracting - Indexing; About IWA Publishing. Subscribe: Institutional
Subscriptions; User Licences; IP Registration; IWA Member c

  Related articles All 2 versions

y~z~…—Ê‚Ì„’è•û–@‚Æ‚µ‚ÄMRR‚Ì—±Œa•ª•z‚©‚ç„’è‚·‚éŽè–@‚ÆZR–@‚ð”äŠr‚µ‚½B—±Œa•ª•z‚©‚焒肵‚½‚Ù‚¤‚ª‚¸“x‚Å‚ ‚Á‚½BMRR‚̓Œ[ƒ_’¼‹ß‚Ì3ƒŒƒ“ƒWƒrƒ“‚͉߬•]‰¿‚·‚éB

 

3Insights into the evolving microphysical and kinematic structure of northeastern US winter storms from dual-polarization Doppler radar

MR KumjianKA Lombardo - Monthly Weather Review, 2017 - journals.ametsoc.org

c Using a vertically pointing Micro Rain Radar (MRR; Peters et al c No thresholds were applied,
in order to preserve 
melting-layer signatures and those from potentially useful signatures such
as the gsnow flare.h For details about the polarimetric radar variables and their physical c

  Cited by 7 Related articles All 4 versions

y¢zWSR88D‚Ì€“V’¸ŠÏ‘ªi‚“x•Ï‰»‚ð‹——£•Ï‰»‚É’u‚«Š·‚¦‚é‰ðÍj‚É‚æ‚è“~‚É‘å‚«‚È~…‚ð‚à‚½‚ç‚·‰_‚ð‰ðÍ‚µ‚½B‘å‚«‚È~…‚ª‚ ‚é‚Æ‚«‚ÍA-15Ž‚ł̃ÓDP‚̕ω»‚ª‚ ‚Á‚½B‚±‚Ì‚Æ‚«’nãŠÏ‘ª‚Å‚Íá‰J”䂪‘å‚«‚©‚Á‚½y—v’²¸zB—Z‰ð‘w‚ª‹}‘¬‚Ɉړ®‚·‚é‚Æ‚«‚Í’nã‚̉Já”»’肪‚¤‚Ü‚­‚¢‚Á‚Ä‚¢‚È‚¢B“ñ•Î”gŠÏ‘ª‚ÌŒ‹‰Ê‚ðƒ‚ƒfƒ‹‚ÉŽæ‚èž‚Ý–k“ŒƒAƒƒŠƒJ‚Ì“~Šú~…‚̉𖾂ɖ𗧂Ăé—\’è‚Å‚ ‚éB

MRR‚Íጋ»icrystal habitj‚Ɖ_—±•t’…‚Ì”»’èA~…‹­“x‚Ì•]‰¿‚É—˜—pB}1‚ÅZe‚̉”’¼•ª•z‚ðWSR88D‚Æ”äŠrB

 

4Rain height information from TRMM precipitation radar and micro rain radar for radio communication studies in Nigeria

JS Ojo, OL Ojo, CI Joseph-Ojo - Adaptive Science & c, 2014 - ieeexplore.ieee.org

c The analysis has been carried out based on the stratiform rain events which normally exhibit
a characterized 
melting layer or bright-band. These results are compared with a measurement
from ground-based vertically looking 
micro rain radar (MRR) and the mean 0oC isotherm c

  Cited by 2 Related articles All 2 versions

[PDF] int-res.com

y~z‰q¯’ÊM‚ÌŒ¸Š‚ð•]‰¿‚·‚邽‚ß‚É0Ž‚“xi—Z‰ð‘w‚“xj‚ªd—v‚Å‚ ‚éBTRMM-PR‚É‚æ‚è0Ž‚“x‚ðŽZ’肵MRR‚Æ”äŠr‚µ‚½B—¼ŽÒ‚Í‚æ‚­ˆê’v‚µ‚½B

 

5Snowfall event characteristics from a high‑elevation site in the Southern Appalachian Mountains, USA

DT Martin, LB Perry, DK Miller, PT Soulé - Climate Research, 2015 - int-res.com

c 1018 1 min Micro Rain Radar (MRR) c Melting layer heights were determined using an automated
algorithm
in the NCSU OPL Viewer Soft- ware (North Carolina State University Department of
Marine, Earth and Atmospheric Sciences, Cloud and Precipitation Processes and c

  Cited by 6 Related articles All 10 versions

y—v’²¸zBB’†‚𒲂ׂĂ¢‚é‚©H

 

[HTML] ametsoc.org

6A Self-Consistent Numerical Method for Microphysical Retrieval in Rain Using GPM Dual-Wavelength Radar

E Gorgucci, L Baldini - Journal of Atmospheric and Oceanic c, 2016 - journals.ametsoc.org

c is preferable because it is more robust and is not influenced by the attenuation of the ice cloud
region and the 
melting layer c Gorgucci and Baldini (2015) implemented a method for transforming
DSD vertical profiles estimated by a vertically pointing 
Micro Rain Radar to a DSD c

  Related articles All 4 versions

y—±Œa•ª•z‚̕ω»z

 

[PDF] noaa.gov

7[PDF] Monitoring Radar Calibration using Ground Clutter

V Melnikov, D Zrnic, A Free, R Macemon - 2017 - nssl.noaa.gov

c 2017). Vertical sensing of precipitation with weather radar and micro-rain radar along with rain
gage measurements are used on the German radar network (Frech et al. 2017) c cloud areas.
It assumes that
snow aggregates exist just above the melting layer thus their ZDR c

  Related articles All 2 versions 

y‹ÃW‰ß’ö‚ª‰½‚ÉŠñ—^‚·‚é‚©Hz

 

[PDF] semanticscholar.org

8[PDF] EARLY ONLINE RELEASE

M Jensen, W Petersen, A Bansemer, N Bharadwajc - 2015 - pdfs.semanticscholar.org

c (ADMIRARI; Saavedra et al. 2011) operated at the ARM Central Facility site with its 19 and 37
173 GHz passive microwave radiometers and a K-band 
Micro Rain Radar to detect and separate
174 contributions to cloud total water content from cloud and rainwater components c

  

y•úŽËŒvz

 

[HTML] ametsoc.org

9The great Colorado flood of September 2013

D Gochis, R SchumacherK Friedrichc - Bulletin of the c, 2015 - journals.ametsoc.org

  Cited by 89 Related articles All 11 versions

yz

 

[HTML] mdpi.com

10[HTML] Real-Time Rain Rate Evaluation via Satellite Downlink Signal Attenuation Measurement

F Giannetti, R Reggiannini, M Moretti, E Adirosic - Sensors, 2017 - mdpi.com

We present the NEFOCAST project (named by the contraction of gNefeleh, which is the Italian
spelling for the mythological cloud nymph Nephele, and gforecasth), funded by the Tuscany Region,
about the feasibility of a system for the detection and monitoring of precipitation fields c

  Related articles All 11 versions 

yƒiƒEƒLƒƒƒXƒgz

 

 

Page6

1Anomalies in relative humidity profile in the boundary layer during convective rain

R ChakrabortyS TalukdarU SahaS Janac - Atmospheric Research, 2017 - Elsevier

c Liquid water content profiles for the study have been taken from Micro Rain Radar
(MRR) observations. MRR c heights. Thus, it is capable of indicating the presence
of 
melting layer by bright band signatures during rain events c

  Cited by 6 Related articles All 6 versions

yz

 

2Rainfall observations and assessment using vertically pointing radar and X-band radar

N Mazari, HO SharifH Xie, AE Tekelic - Journal of c, 2017 - jh.iwaponline.com

Skip to main content. Main menu. About the Journal: Aims & Scope; Editorial Board;
Browse Archive; Abstracting - Indexing; About IWA Publishing. Subscribe: Institutional
Subscriptions; User Licences; IP Registration; IWA Member c

  Related articles All 2 versions

yz

 

3Insights into the evolving microphysical and kinematic structure of northeastern US winter storms from dual-polarization Doppler radar

MR KumjianKA Lombardo - Monthly Weather Review, 2017 - journals.ametsoc.org

c Using a vertically pointing Micro Rain Radar (MRR; Peters et al c No thresholds were applied,
in order to preserve 
melting-layer signatures and those from potentially useful signatures such
as
the gsnow flare.h For details about the polarimetric radar variables and their physical c

  Cited by 7 Related articles All 4 versions

y~á‚Ì‹}”­’Bz

 

4Rain height information from TRMM precipitation radar and micro rain radar for radio communication studies in Nigeria

JS Ojo, OL Ojo, CI Joseph-Ojo - Adaptive Science & c, 2014 - ieeexplore.ieee.org

c The analysis has been carried out based on the stratiform rain events which normally exhibit
a characterized 
melting layer or bright-band. These results are compared with a measurement
from ground-based vertically looking micro rain radar 
(MRR) and the mean 0oC isotherm c

  Cited by 2 Related articles All 2 versions

yMRR‚ÍŒŸØ‚É—˜—pz

 

[PDF] int-res.com

5Snowfall event characteristics from a high‑elevation site in the Southern Appalachian Mountains, USA

DT Martin, LB Perry, DK Miller, PT Soulé - Climate Research, 2015 - int-res.com

c 1018 1 min Micro Rain Radar (MRR) c Melting layer heights were determined using an automated
algorithm in the NCSU OPL Viewer Soft- ware
(North Carolina State University Department of
Marine, Earth and Atmospheric Sciences, Cloud and Precipitation Processes and c

  Cited by 6 Related articles All 10 versions

[HTML] ametsoc.org

yŽR’n•”‚É‚¨‚¯‚é~á‰_‚Ì“Á’¥z

 

6A Self-Consistent Numerical Method for Microphysical Retrieval in Rain Using GPM Dual-Wavelength Radar

E Gorgucci, L Baldini - Journal of Atmospheric and Oceanic c, 2016 - journals.ametsoc.org

c is preferable because it is more robust and is not influenced by the attenuation of the ice cloud
region and the 
melting layer c Gorgucci and Baldini (2015) implemented a method for transforming
DSD vertical profiles
estimated by a vertically pointing Micro Rain Radar to a DSD c

  Related articles All 4 versions

y‘OoH—±Œa•ª•z‚̕ω»z

 

[PDF] noaa.gov

7[PDF] Monitoring Radar Calibration using Ground Clutter

V Melnikov, D Zrnic, A Free, R Macemon - 2017 - nssl.noaa.gov

c 2017). Vertical sensing of precipitation with weather radar and micro-rain radar along with rain
gage measurements are used on the German radar network (Frech et al. 2017) c cloud areas.
It assumes that
snow aggregates exist just above the melting layer thus their ZDR c

  Related articles All 2 versions 

y‹ÃW‚ÌŠñ—^z

 

[PDF] semanticscholar.org

8[PDF] EARLY ONLINE RELEASE

M Jensen, W Petersen, A Bansemer, N Bharadwajc - 2015 - pdfs.semanticscholar.org

c (ADMIRARI; Saavedra et al. 2011) operated at the ARM Central Facility site with its 19 and 37
173 GHz passive microwave radiometers and a K-band 
Micro Rain Radar to detect and separate
174 contributions to cloud total water content from cloud and rainwater components c
 

y48‚Æ“¯‚¶B•úŽËŒv‚ð—˜—pz

 

[HTML] ametsoc.org

9The great Colorado flood of September 2013

D Gochis, R SchumacherK Friedrichc - Bulletin of the c, 2015 - journals.ametsoc.org

  Cited by 89 Related articles All 11 versions

yz

 

[HTML] mdpi.com

10[HTML] Real-Time Rain Rate Evaluation via Satellite Downlink Signal Attenuation Measurement

F Giannetti, R Reggiannini, M Moretti, E Adirosic - Sensors, 2017 - mdpi.com

We present the NEFOCAST project (named by the contraction of gNefeleh, which is the Italian
spelling for the mythological cloud nymph Nephele, and gforecasth), funded by the Tuscany Region,
about
the feasibility of a system for the detection and monitoring of precipitation fields c

  Related articles All 11 versions 

y—\‘ªƒVƒXƒeƒ€B50‚Æ“¯‚¶z

 

 

Page7

‚PThe CHUVA project: How does convection vary across Brazil?

LAT Machado, MAF Silva Diasc - Bulletin of the c, 2014 - journals.ametsoc.org

c These data include 1) the selected cloud properties from X-band dual-polarization radar (X-Pol)
and 
Micro Rain Radar (MRR) data; 2) satellite and radar precipitation fields, cloud-type
classification, and cloud and rain cell life cycles; 3) the electric fields and lightning associated c

  Cited by 54 Related articles All 12 versions

yƒvƒƒWƒFƒNƒg‚Ìà–¾z

 

[HTML] ametsoc.org

2A W-Band Radar–Radiometer System for Accurate and Continuous Monitoring of Clouds and Precipitation

N Küchler, S Kneifel, U Löhnertc - c of Atmospheric and c, 2017 - journals.ametsoc.org

c 2013) or for investigating processes with strong vertical gradients (eg, melting layer). The
increased time on target, because of continuous transmission, provides similar average output
powers as pulsed systems and leads to comparable sensitivities c

  Related articles All 3 versions

yƒuƒ‰ƒCƒgƒoƒ“ƒh‚ÌŒŸoz

 

[HTML] ametsoc.org

3WRF–SBM simulations of melting-layer structure in mixed-phase precipitation events observed during LPVEx

T IguchiT MatsuiWK TaoAP Khainc - Journal of Applied c, 2014 - journals.ametsoc.org

c WRF–SBM Simulations of Melting-Layer Structure in Mixed-Phase Precipitation Events Observed
during LPVEx c The detailed ice-melting scheme with prognosis of the liquid water fraction during
melting enables explicit
simulation of microphysical properties in the melting layer c

  Cited by 6 Related articles All 7 versions

yWRFƒrƒ“ƒ‚ƒfƒ‹‚É‚æ‚鬇‰_‚ÌŒŸØGMRR‚Í—±ŒaƒXƒyƒNƒgƒ‹ŒŸoz

 

[PDF] ursi.org

4Earth-space Propagation through rain and associated tropospheric processes at a tropical location

A Maitra, A Adhikari, T Sarkarc - General Assembly and c, 2014 - ieeexplore.ieee.org

c For the study of the vertical rain structure, a Micro Rain Radar (MRR), a vertically pointing
FM-CW radar at 24.1 GHz, has been operated at the same site.
The vertical profile of rain rate
and radar reflectivity
can indicate the presence of melting layer with bright band signatures c

  Related articles All 6 versions

y—Z‰ð‘w‚ÌŒ¸ŠŒø‰Êz

 

[HTML] ametsoc.org

5A method to estimate the 3D–time structure of the raindrop size distribution using radar and disdrometer data

M Schleiss, J Smith - Journal of Hydrometeorology, 2015 - journals.ametsoc.org

c Next section. A geostatistical method to quantify the small-scale 3D–time structure of the drop size distribution (DSD) from the ground level up to the melting layer using radar and disdrometer data is presented c

  Cited by 4 Related articles All 6 versions

y—Z‰ð‘w‚æ‚艺‚Ì—±Œa•ª•z•Ï‰»z

 

6The characteristics of precipitation observed over Cypress Mountain during the SNOW-V10 campaign

HWS Berg, RE Stewart, PI Joe - Atmospheric Research, 2017 - Elsevier

c Data from a vertically-pointing Micro Rain Radar (MRR) at West Vancouver were obtained
between January 22 and April 29 to examine the vertical structure of precipitating systems (Joe
et al., 2014) c In addition,
the melting layer is evident in these figures, for example in Fig c

  Related articles All 2 versions

[PDF] ursi.org

y—Z‰ð‘w‚ðŠÜ‚Þ~…‚̉”’¼•ª•z‚Ì“Á’¥z

 

7Ka-band radar observations of tropical rain features

S DasA Maitra - c and Scientific Symposium (URSI GASS), 2014 c, 2014 - ieeexplore.ieee.org

c The bias in vertical profile of reflectivity arises due to the assumptions of constant reflectivity up
to melting layer 
from surface c In this paper, observations of vertical rain structure obtained using
vertical looking Ka band radar (
Micro Rain Radar -MRR) at Ahmedabad (23‹04', 73‹38 c

  Related articles All 6 versions

y—Z‰ð‘w‚æ‚艺‚Ì~…•ª•z‚ÆŒ¸Š—Êz

 

8Advances in Clouds and Precipitation Modeling Supported by Remote Sensing Measurements

T Iguchi, T Matsui - Remote Sensing of Clouds and Precipitation, 2018 - Springer

c CFTDs of the water equivalent radar reflectivity factor (dBZ) derived from the micro rain radar
measurements at the Jarvenpaa site coupled with the vertical temperature c WRF-SBM simulations
of 
melting-layer structure in mixed-phase precipitation events observed during LPVEx c

  All 3 versions

y63‚Æ“¯“à—eBWRF-SBMiƒXƒyƒNƒgƒ‹ƒrƒ“ƒ‚ƒfƒ‹G~áŽí‚Í6ŒÂjz

 

[HTML] wiley.com

9[HTML] Microphysics of clouds and rain over the Western Ghat

M KonwarSK Das, SM Deshpandec - Journal of c, 2014 - Wiley Online Library

c One Micro Rain Radar (MRR) and OTT PARSIVEL disdrometer (PD) is located at IITM-. The X
band radar was
operated in 2012 during the monsoon season. The HACPL is located at
Mahabaleshwar (17.92‹N, 73.66‹E, above sea level 1.39 km) established in 2012 c

  Cited by 17 Related articles All 5 versions

yMRR‚ÆPSV2‚Ì“¯ŽžŠÏ‘ªz

 

[HTML] ametsoc.org

10Empirical relationships for estimating liquid water fraction of melting snowflakes

R Misumi, H Motoyoshi, S Yamaguchic - Journal of Applied c, 2014 - journals.ametsoc.org

c When snowflakes fall through a melting layer, high radar reflectivity occurs and a bright band
can be observed c A vertical-pointing K-band radar [Meteorologische Messtechnik GmbH (METEK)
Micro Rain Radar] was also used to obtain vertical profiles of radar reflectivity at 50-m c

  Cited by 6 Related articles All 11 versions

 

y—ZáŒv‚É‚æ‚éŠÏ‘ªz

 

 

Page8

1Cloud and rain liquid water statistics in the CHUVA campaign

AJP Calheiros, LAT Machado - Atmospheric research, 2014 - Elsevier

c LWC R ) profiles were determined using the vertical profiles of reflectivity (VPR) of the two radar
systems, 
Micro Rain Radar (MRR, Peters et al c analyses, one for non-precipitating events and
another for clouds with rain, describing the cloud characteristics below the 
melting layer c

  Cited by 10 Related articles All 12 versions

y~—Z‰ð‘wˆÈ‰º‚Ì~…—ÊŠÏ‘ªŠÏ‘ªz

 

2Characteristics of summer and winter precipitation over northern China

G Wen, H Xiao, H Yang, Y Bi, W Xu - Atmospheric Research, 2017 - Elsevier

c data. Abstract. In this paper, the statistical properties of summer and winter
precipitation over the northern China plain are investigated by using a
two-dimensional video disdrometer (2DVD) and a 
micro-rain radar (MRR). The c

  Related articles All 2 versions

y~~…“Á«‚Ì“Œv’lz

 

3Observation of a freezing drizzle episode: A case study

S Fernández-González, F Valero, JL Sanchezc - Atmospheric c, 2014 - Elsevier

c nuclei. Keywords. Freezing drizzle. Cloud chamber. Radiometer. Micro Rain Radar-2.
MSG. 1. Introduction c 2007). 3.3. 
Micro Rain Radar (MRR-2). The MRR-2 operates with
electromagnetic radiation at K-band, with frequency 24.230 GHz c

  Cited by 12 Related articles All 5 versions

yŸz“€‰J‚Ì”­¶‚ɂ‚¢‚Ä

 

4Temporal and structural evolution of a tropical monsoon cloud system: A case study using X-band radar observations

SK Das, SM Deshpande, SS DasM Konwarc - Journal of Atmospheric c, 2015 - Elsevier

c Observations from a vertically pointing Micro Rain Radar (MRR) and cloud profiling radar (CPR)
onboard CloudSat suggested occurrence of both shallow c Zawadzki (1995) by using the X-band
radar observations studied the profiles of reflectivity factors near the 
melting layer c

  Cited by 3 Related articles All 5 versions

y¢”M‘т̉_~…‰ß’ö‚ɂ‚¢‚Äz

 

5Observation of bright-band height data from TRMM-PR for satellite communication in South Africa

EO Olurotimi, O Sokoya, JS Ojo, PA Owolawi - Journal of Atmospheric and c, 2017 - Elsevier

c overall poor quality of service (QoS). Often time, rain height information is obtained
indirectly from the 
melting layer zone of the atmosphere (Das and Maitra, 2011; Yussuff
and Khamis, 2013). Since direct rain height data measurement c

  Related articles All 2 versions

y~‰q¯’ÊM‚Ì‚½‚ß‚ÌTRMM-PR‚É‚æ‚é0Ž‚“x‚Ì„’èz

 

[PDF] researchgate.net

6Observational study on melting layer characteristics over Palau in Pacific Ocean

UVM Krishna, KK Reddy, R Mastanaiahc - Journal of Atmospheric c, 2014 - Elsevier

c However, modeling of melting layer/bright band either obtains correct reflectivity enhancement
or overestimate the intensity c JAMSTEC installed ground based sensors viz., a Lower Atmospheric
Wind Profiler (LAWP), 
Micro Rain Radar, Ceilometer, Microwave Radiometer, Joss c

  Cited by 3 Related articles All 4 versions

y~ƒpƒ‰ƒI‚Å‚ÌTRMM-PR‚É‚æ‚é0Ž‚“x‚Ì„’èzƒGƒ‹ƒj[ƒjƒ‡Žž‚Ì—Z‰ð‘qŒÉ“x•Ï‰»‚Ì“Á’¥B

 

[PDF] researchgate.net

7[PDF] Dual-polarization radar particle classification results during the Sochi Olympic Games

J Reid, D Hudak, S Boodoo, N Donaldsonc - ERAD 2014, the c, 2014 - researchgate.net

c In the future, particle type validation can be furthered by examining vertically profiling
Micro Rain Radar (MRR) data from 2 Sochi-area sites. Melting layer information and
fall speeds from the MRR may help discern particle type c

  Cited by 3 Related articles All 4 versions 

y~Cƒoƒ“ƒhƒŒ[ƒ_‚É‚æ‚é—±Žq”»•Êzparticle classification algorithm (PCA) MRR‚ÍŒŸØ‚É—˜—pB

 

[HTML] ametsoc.org

8Role of a Cross-Barrier Jet and Turbulence on Winter Orographic Snowfall

J Aikins, K Friedrich, B Geertsc - Monthly Weather c, 2016 - journals.ametsoc.org

c A suite of high-resolution radars, including a ground-based scanning X-band dual-polarization
Doppler on Wheels radar, vertically pointing Ka-band 
Micro Rain Radar (MRR), and airborne
W-band Wyoming Cloud Radar (WCR), and additional in situ and remote sensing c

  Cited by 1 Related articles All 5 versions

y¢’nŒ`‚É‚æ‚é‹C—¬‚ÌŽû‘©‚̉e‹¿’²¸zMRR‚͉_‚ª”­¶‚µ‚Ä‚¢‚éã‹ó‚𒲂ׂ½B

 

[HTML] ametsoc.org

9A shallow cumuliform snowfall census using spaceborne radar

MS Kulie, L Milani, NB Woodc - Journal of c, 2016 - journals.ametsoc.org

c This assumed melting layer depth enables snowfall retrievals to be made for surface temperatures
up to ~1.5‹C. The 2C-SNOW-PROFILE optimal estimation scheme is constrained by a priori snow
microphysical properties (eg, observed mass–size relationships and particle c

  Cited by 9 Related articles All 4 versions

y¢‰_ŠÏ‘ª‰q¯‚É‚æ‚é~…‰_‚Ì•]‰¿zCloudSat‚̃Aƒ‹ƒSƒŠƒYƒ€‚ð—p‚¢‚½‰_ƒ^ƒCƒv‚Æ~áˆæ‚Ì‘S‹…“I•]‰¿B”–‚¢~á‰_‚Å‚ ‚éA‘wω_‚Ü‚½‚Í—‘w‰_‚©‚ç‚Ì~…‚ª~á‚Ì36“A59“‚ðè‚ß‚éB

 

[HTML] wiley.com

10[HTML] How does the spaceborne radar blind zone affect derived surface snowfall statistics in polar regions?

M Maahn, C Burgard, S Crewellc - Journal of c, 2014 - Wiley Online Library

c In this study, the impact of the blind zone of CloudSat on derived snowfall statistics in polar regions
is investigated by analyzing three 12 month data sets recorded by ground-based 
Micro Rain
Radar (MRR) at the Belgian Princess Elisabeth station in East Antarctica and at Ny c

  Cited by 11 Related articles All 4 versions

y~MRR‚ÌŠÏ‘ª‚ð—p‚¢‚ÄCloudSat‚ÌŠÏ‘ª•s”\ˆæ‚ðŒyŒ¸‚·‚ézSvalbard, Norway

 

 

Page9

1Invariance of the double-moment normalized raindrop size distribution through 3D spatial displacement in stratiform rain

TH RaupachA Berne - Journal of Applied Meteorology and c, 2017 - journals.ametsoc.org

  Cited by 1 Related articles All 4 versions

y¢‘wó«Ì‘Η¬«‚̕ω»‚É‚¨‚¯‚é2ŽŸƒ‚[ƒƒ“ƒg—±Œa•ª•z‚Ì•Û‘¶«z‰_‚̃^ƒCƒv‚ª•Ï‰»‚·‚éÛ‚É2ŽŸƒ‚[ƒƒ“ƒgi—±ŒaAŒÂ”j—±Œa•ª•z‚ª3ŽŸŒ³‹óŠÔ•ª•z‚Å•]‰¿‚µ‚Ä•s•Ï‚Å‚ ‚邱‚Ƃ̉ðÍBMRR‚ÍDSD‚Ì‚“x•Ï‰»‚𒲸B

 

[PDF] archives-ouvertes.fr

2 4-D-VAR assimilation of disdrometer data and radar spectral reflectivities for raindrop size distribution and vertical wind retrievals

F Mercier, A Chazottesc - Atmospheric c, 2016 - hal-insu.archives-ouvertes.fr

c Then, we present the characteris- tics of the case study examined. 3.1 Micro-rain radar (MRR)
The first instrument used in this study is a 
micro-rain radar (MRR, Peters et al., 2005), developed
by METEK GmbH, Germany, and belonging to Météo France c

  Related articles All 11 versions

y~Žã‚¢‘wó«‚Ì~‰J‚ÉŒÀ’肵‚Ä‚SDV‚ðŒŸØ‚µ‚½z•¡”Ž–—á‚ð’Šo‚·‚éÛA2~7mm/h‚Ì~‰J‚Æ—±Œa•ª•z‚̃f[ƒ^ƒZƒbƒg‚ðì‚邽‚ß‚ÉMRR‚ð—˜—pB

 

3 Improving Polarimetric C-Band Radar Rainfall Estimation with Two-Dimensional Video Disdrometer Observations in Eastern China

G Chen, K Zhao, G Zhang, H Huangc - Journal of c, 2017 - journals.ametsoc.org

c We specifically chose data from all vertically pointing data below the melting layer
in light rain to calculate the Z DR biases for Z DR calibration in every IOP. The Z DR
biases vary between 0.3 and 0.5 dB throughout the OPACC c

  Related articles All 3 versions

DSD’²¸‚É‚æ‚éQPE‚ÌŒüãz‘ä•—‚â‘Oü‚É”ä‚ׂăXƒR[ƒ‹ƒ‰ƒCƒ“‚Ì•Ï“®‚ª‘å‚«‚¢BƒXƒR[ƒ‹ƒ‰ƒCƒ“‚Å‚Í‘O2ŽÒ‚É”ä‚ׂđ嗱Žq‚ª‘¶Ý‚µA‘å—±Žq‚Ì”–§“x‚Ì•Ï“®‚É‚æ‚Á‚ÄQPE‚̸“x‚ª•Ï“®‚·‚éB

 

4 4-D-VAR assimilation of disdrometer data and radar spectral reflectivities for rain drop size distribution and vertical wind retrievals.

F Mercier, A Chazottes, L Barthèsc - Atmospheric c, 2015 - search.ebscohost.com

Page 1. AMTD 8, 12383–12431, 2015 Vertical variability of DSD F. Mercier et al. Title Page c

  Related articles All 2 versions

y~㸗¬‚ðl—¶‚µDSD‚Ì„’è‚ðŒüãz—±Žq‚Ì•¹‡A…•½ˆÚ“®‚Í–³Ž‹BŽã‚¢‰J‚ÉŒÀ’èBMRR‚ÍŽ–—á‘I‘ð‚É—˜—pB

 

5 [PDF] unand.ac.id

5Struktur Vertikal Distribusi Butiran Hujan di Kototabang Berdasarkan Pengamatan Micro Rain Radar (MRR)

I Rahayu, M MarzukiH Hashiguchic - Jurnal Fisika c, 2016 - jfu.fmipa.unand.ac.id

c Untuk mengatasi kekurangan radar pulsa, telah dikembangkan radar dengan gelombang
kontinyu seperti 
Micro Rain Radar (MRR) (Peters dkk., 2002) c Lapisan ini disebut melting
layer dimana partikel es mulai mencair menjadi butiran hujan c

  Related articles All 2 versions

yz

 

6Shallow Precipitation Detection and Classification Using Multifrequency Radar Observations and Model Simulations

M ArulrajAP Barros - Journal of Atmospheric and Oceanic c, 2017 - journals.ametsoc.org

c The IPHEx IOP was conducted between 1 May 2014 and 15 June 2014 over the southeastern
United States with collocated instruments installed at MV (35.5198‹N, 83.0947‹W), including
a scanning W-band dual-polarization radar, a 
Micro Rain Radar (MRR), an all-sky imager c

  Related articles All 3 versions

y~z”–‚¢’g‚©‚¢‰_yNonBrightBandRainz‚̓Šƒ‚[ƒgƒZƒ“ƒVƒ“ƒOŒë·‚Æ‚È‚éB‘½”g’·‚ÌŠÏ‘ª‚É‚æ‚èƒAƒ‹ƒSƒŠƒYƒ€‚̉ü‘P‚ð}‚Á‚½B

 

7[PDF] researchgate.net

7Raindrop size distributions of southwest and northeast monsoon heavy precipitation observed over Kadapa (14‹ 4Œ N, 78‹ 82Œ E), a semi-arid region of India

J Jayalakshmi, KK Reddy - Current Science, 2014 - JSTOR

c Raindrop size distributions (RSD) of southwest (SW - June to September) and northeast (NE -
October to December) monsoon heavy precipitation are measured with PARticle Size and
VELocity (PARSIVEL) dis drometer and 
Micro Rain Radar (MRR) deployed at Kadapa (14.47 c

y~z“켃‚ƒ“ƒX[ƒ“y‰ÄzA–k“Œƒ‚ƒ“ƒX[ƒ“y“~z‚Ì—±Œa•ª•z‚𒲂ׂ½B“켃‚ƒ“ƒX[ƒ“‚łͬ—±Œa‚ª­‚È‚©‚Á‚½B

 

  Cited by 6 Related articles All 2 versions

[PDF] duke.edu

8[PDF] NASA GPM-Ground Validation: Integrated Precipitation and Hydrology Experiment 2014 Science Plan.

A Barros, W Petersen, M Schwaller, R Cifellic - 2014 - dukespace.lib.duke.edu

c In the rain, vertical profiles of drop size distributions from the melting layer down to the ground
surface as well as robust estimates of path-integrated-attenuation at high spatial resolution that
can be used for the parameterization of microphysical processes will provide a critical c

  Cited by 9 Related articles All 3 versions 

y~zGMPŒŸØ‚ÌŒv‰æ‘BMRR‚ÍŽd—l‚Ìà–¾‚Ì‚ÝB

 

[HTML] wiley.com

9[HTML] A comparison study of summer season raindrop size distribution between Palau and Taiwan, two Islands in Western Pacific

BK Seela, J Janapati, PL Lin, KK Reddyc - Journal of c, 2017 - Wiley Online Library

By continuing to browse this site you agree to us using cookies as described
in About Cookies. Remove maintenance message c

  Related articles All 2 versions

y~zƒpƒ‰ƒI‚Æ‘ä˜p‚Å‚Ì—±Œa•ª•z”äŠrB‘ä˜p‚ł̓pƒ‰ƒI‚æ‚è’†‘å—±Žq‚ª‘½‚¢B

 

[PDF] uncg.edu

10[PDF] Radar-observed Characteristics of Precipitation in the Tropical High Andes of Southern Peru and Bolivia

JL Endries - 2017 - libres.uncg.edu

c southern Peru and Bolivia. A vertically pointing 24.1 GHz Micro Rain Radar in Cusco, Peru c
These data enabled the determination of precipitation timing and 
melting layer heights and
the identification of convective and stratiform precipitation features c

  Related articles All 3 versions 

y~zMRR‚ð—Z‰ð‘w‚“x‚Ì”»’è‚É—˜—p‚µ~…‚ÌŠJŽn‚ð”»’fB

 

 

Page10

1Precipitation microstructure in different Madden–Julian Oscillation phases over Sumatra

H Hashiguchi, T Kozu, T Shimomai, Y Shibagakic - Atmospheric c, 2016 - Elsevier

c The characteristics and performance of the EAR were provided in detail by Fukao et al. (2003).
The vertical profile of DSD was observed by using 24 GHz 
micro-rain radar (MRR) data.
Simultaneous observation of MRR and 2DVD were not available c

  Cited by 7 Related articles All 3 versions

y¢ƒ}ƒbƒfƒ“ƒ“ƒWƒ…ƒŠƒAƒ“Šú‚É‚¨‚¯‚é—±Œa•ª•z‚̕ω»zŠˆ«Šú‚Í[‚¢‘Η¬‚ª‘½‚­”ñŠˆ«Šú‚ÍŽã‚¢‘Η¬‚ª‘½‚¢B”ñŠˆ«Šú‚Å‚Í’†E‘å—±Žq‚Ì””Z“x‚ª‘½‚¢B‚±‚Ì‚½‚ß“¯‚¶~…‹­“x‚Å‚àZ‚ª‘å‚«‚­‚È‚éB

 

2 [BOOK] Chilean coastl orographic precipitation experiment: A tale of two rain regimes

AK Massmann - 2016 - search.proquest.com

c 24. correct classications is minimized. Incorrect classications are dened as half-hour
periods in which the MRR either falsely detects a 
melting layer or fails to detect a melting
layer c 210m and 35% of proles required to identify a melting layer c

  Related articles All 2 versions

y~–{‚Ì–`“ª•”•ª‚Éz’nŒ`«~‰J‚ð‰ðÍ‚·‚邽‚ß‚ÌW’†ŠÏ‘ª‚Ìà–¾B~…‚̉”’¼•ª•z‚ðŠÏ‘ª‚·‚邽‚ß‚ÉMRR‚ð—˜—p

 

[PDF] altostratus.it

3Overview of the first HyMeX Special Observation Period over Italy: observations and model results

R Ferretti, E Pichelli, S Gentile, I Maielloc - c and Earth System c, 2014 - search.proquest.com

c These include an X-band polarimetric mini-radar, a K-band microrain radar and several
disdrometers of three kinds, namely, a 2-D video disdrometer, PLUDIX, and laser Parsivel-2
disdrometers (see Table 1). The LT hydro-meteorological site is located at the east- ern c

  Cited by 37 Related articles All 14 versions

y~^…‚̂悤‚È‘å‰J‚ð‚à‚½‚ç‚·‰_‚ɂ‚¢‚Ä‚ÌLˆæŠÏ‘ª‚ɂ‚¢‚ă‚ƒfƒ‹‚ÆŠÏ‘ª‚Ì”äŠrz

 

[PDF] academia.edu

4Weather observations on Whistler Mountain during five storms

2014 - Springer JM ThériaultKL Rasmussen, T Fisicoc - Pure and Applied c,

c A micro rain radar (MRR) was also available to detect precipitation type and reflectivity c 13c). Finally,
the temperature profiles measured on 10 March differed slightly and suggest the presence of
melting layer at lower elevations (Fig. 14a, c). Open image in new window. Fig. 13 c

  Cited by 4 Related articles All 13 versions

y›•¡ŽG’nŒ`‰º‚Ì~…Œ`¬‰ß’öz‘ŠÏê‚̈قȂé5—á‚ð‰ðÍB0“xˆÈ‰º‚É‚à‚©‚©‚í‚炸‰J‚©‚çá‚Ö‚Ì‘JˆÚ‚Í2—Ⴕ‚©ŠÏ‘ª‚Å‚«‚È‚©‚Á‚½B

 

[PDF] bibsys.no

5Estimation of ZR relationship and comparative analysis of precipitation data from colocated rain-gauge, vertical radar and disdrometer

I Cyr - 2014 - brage.bibsys.no

c The main objective of this study is to estimate storm type and precipitation phase dependent ZR
parameters from optical disdrometer (OTT Parsivel) and 
Micro Rain Radar (MRR) measurements
which can be used to convert Z values extrapolated from C-band radar c

  Cited by 3 Related articles All 3 versions

y¢’nã‰J—ÊŒvAPSV2‚ÆMRR‚Ì”äŠrA‰JAáA¬‡‰_‚ª‘ÎÛz¬‡‰_‚ɂ‚¢‚Ä‚ÍAÏŽZ‚·‚é‚Æ’nã‰J—ÊŒv‚ÆPSV2‚ªˆê’v‚·‚éB

 

[PDF] atmos-meas-tech.net

6Retrieval of the raindrop size distribution from polarimetric radar data using double-moment normalisation

TH Raupach, A Berne - Atmospheric Measurement c, 2017 - search.proquest.com

c Also used. were data from a METEK GmbH micro rain radar (MRR. Peters et al., 2002, 2005;
Tridon et al., 2011) within the net c Peters, G., Fischer, B., and Andersson, T.: Rain observations
with. a vertically looking 
Micro Rain Radar (MRR), Boreal Environ. Res., 7, 353–362, 2002 c

  Cited by 1 Related articles All 7 versions

y~2ŽŸƒ‚[ƒƒ“ƒg‚Ì—±Œa•ª•z‚Ì••Õ«‚ð—p‚¢‚½V‚½‚È—±Œa•ª•z‚Ì„’è–@‚ð’ñˆÄz81‚Æ“¯‚¶’˜ŽÒB

 

[PDF] colostate.edu

7RAdar multi-sensor (RAMS) quantitative precipitation estimation (QPE)

DD Willie - 2015 - dspace.library.colostate.edu

c 146 Figure 8.15 Micro Rain Radar c Designed to cover the entire continental US •Radar reflectivity requires much clutter filtering • Scans above the melting layer require reflectivity correction • Developed to work with NEXRAD c

  Related articles

y~WillieŽ‚ÌD˜_z•¡”‚̃Œ[ƒ_‚ð—p‚¢‚ÄŽÕ•Áˆæ‚̸“x‚ð‚‚ß‚éB

 

[PDF] whiterose.ac.uk

8Quantifying uncertainty in radar rainfall estimates using an X-band dual polarisation weather radar

DRL Dufton - 2016 - etheses.whiterose.ac.uk

c MAPD Mean absolute percentage difference Md median MPD Mean percentage difference MRR
micro rain radar NCAS National Centre for Atmospheric Science NCP normalised coherent power
NERC Natural Environment Research Council PPI plan position indicator xxi c

  Related articles All 3 versions

y~Œ¸Š‚âŽÕ•Á‚ɑ΂·‚éV‚½‚È•â³–@‚Ì’ñˆÄz“ñ•Î”g‚ð—˜—pB

 

[PDF] umanitoba.ca

9Characteristics and formation of precipitation over the Kananaskis Emergency Site during March and April 2015

I Hung - 2016 - mspace.lib.umanitoba.ca

Page 1. Characteristics and Formation of Precipitation over the Kananaskis Emergency Site during
March and April 2015 by Ida Hung A Thesis submitted to the Faculty of Graduate Studies of The
University of Manitoba in partial fulfilment of the requirements of the degree of c

  Related articles All 2 versions

y¢ŽR–¬•—‰º‚Å‚Ì~…—±Žq‚Ì•ª—ÞzƒƒbƒL[ŽR–¬B‰æ‘œ‰ðÍB’ቷŒ^ጋ»‚à‚ ‚èBMRR‚ÍŽg‚Á‚Ä‚¢‚È‚¢iP119j

 

[PDF] umanitoba.ca

On Winter Precipitation at Cypress Mountain, British Columbia, during SNOW-V10

HWS Berg - 2015 - mspace.lib.umanitoba.ca

c Specialized radar showed changes in reflectivity values with height, yielded
information regarding 
melting layer heights, and detected upward motion of
precipitation particles c 3.1.6 
Micro Rain Radar ccccc23 c

  Related articles All 2 versions

y¢ŽR’n•”‚Å‚Ì~áŠÏ‘ªz~᎖—á‚ÌЉîBNOW-V10‚Í42,66‚Å‚àŽÀŽ{‚ÌŒv‰æB

Page11

1구름씨뿌리기에 의한 구름 강수의 미세물리변화 분석

양하영C 채상희C 고아름C 최지원C 이정호c - 한국기상학회 학술대회 c, 2016 - dbpia.co.kr

c J. Appl. Meteor., 27, 1166-1182. Cha. J. W., SS Yum, K. H. Chang and S. N. Oh, 2007: Estimation
of the 
melting layer from a Micro Rain Radar (MRR) data at the Cloud Physics Observation System
(CPOS) site at Daegwallyeong weather station. J. Korean Fig c

  Related articles

yz

 

2산악 지형에서의 지상기반 빙정핵 시딩효과 검증을 위한 MRR PARSIVEL 우적계의 관측사례 분석

양하영C 정진임C 서성규C 장기호c - 한국기상학회 학술대회 c, 2015 - dev02.dbpia.co.kr

c 5. 참고문헌 Cha, JW, SS Yum, KH Chang, and SN Oh, 2007: Estimation of the melting layer
from a 
Micro Rain Radar (MRR) data at the Cloud Physics Observation System (CPOS) site
at Daegwallyeong Weather Station. J. Korean Meteoro. Soc., 43, 77-85 c

  Related articles All 2 versions

yz

 

[PDF] bppt.go.id

3c HUJAN DAN AWAN-AWAN PENGHASIL CURAH HUJAN HARIAN TINGGI DI WILAYAH DRAMAGA, BOGOR BERDASARKAN DATA MICRO RAIN RADAR (MRR)

SA Syafira, D Syaifullahc - Jurnal Sains & Teknologi c, 2016 - ejurnal.bppt.go.id

c Dalam proses pengujian tersebut MRR juga memperlihatkan ketinggian lapisan gmelting layerh
dan perubahannya, yang digunakan sebagai c Pada lokasi inilah dioperasikan seperangkat
instrumen 
Micro Rain Radar (MRR) sebagai penghasil data utama dalam penelitian pada c

  Related articles

y~zƒ{ƒ‹ƒOˆæ‚Ì“ú~…—ʂ͂قڑΗ¬«‚Ì~…‚É‚æ‚é‚à‚Ì‚Å‚ ‚Á‚½B

 

[PDF] uni-stuttgart.de

4Detection of the bright band with a vertically pointing k-bandradar

T Pfaff, A Engelbrecht, J Seidel - 2014 - elib.uni-stuttgart.de

c investigate three different methods to identify the bright band from profiles measured by a vertically
pointing K- Band 
Micro Rain Radar (MRR c BATTAN (1973) states several processes during the
pas- sage of the hydrometeors through the 
melting layer (ie around and below the 0 c

  Cited by 4 Related articles All 6 versions

y¢z3Ží‚Ì—Z‰ð‘wiƒuƒ‰ƒCƒgƒoƒ“ƒhj”»’èŽè–@‚𒲂ׂ½B“K—pŠÖ”‚ð—p‚¢‚é‚à‚ÌAZ‚Ì‚Ý‚ÌŽè–@AW‚ð‰Á–¡‚·‚éŽè–@BƒhƒCƒcŒêB

 

[PDF] uqam.ca

5Étude de la ligne pluie-neige dans la vallée de Kananaskis, Alberta

É Poirier - 2017 - archipel.uqam.ca

c 22 1.5 R-ficctivity measurcd by the Micro Rain Radar at th KES site n 31 Mar h 2015 c Mesas
ale Alpine Pr gram Monte Carlo Indcpendcnt Column Approximati n Madel run without cooling
due to melting 
Micro Rain Radar akiska ski arca North Amcrican Regional Reanalysis c

  All 2 versions

yÚ‘±•s‰Âz

 

[PDF] atmos-meas-tech.net

6A spectral method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted solar radiance spectra

SE LeBlanc, P Pilewskie, KS Schmidtc - Atmospheric c, 2015 - atmos-meas-tech.net

c ra- diation and precipitation. The instruments that provided data for this study are
the pyranometer, pyrgeometer, ceilometer, 
micro rain radar (MRR), sky webcam, and
spectral sunpho- tometer. The pyranometer and pyrgeometer c

  Cited by 12 Related articles All 11 versions

y~‰_‚ÌŒõŠw“IŒú‚³‚Æ—LŒø—±Œa‚ÌŽZ’è–@‚Ì’ñˆÄz

 

[PDF] researchgate.net

7The Impact of Microstructure on an Accurate Snow Scattering Parameterization at Microwave Wavelengths

R Honeyager - 2017 - search.proquest.com

The Impact of Microstructure on an Accurate Snow Scattering Parameterization at
Microwave Wavelengths. Abstract. High frequency microwave instruments are
increasingly used to observe ice clouds and snow. These instruments c

  Related articles All 3 versions

y~Œ`󂪈قȂéá—±Žq‚ɂ‚¢‚Ä‚Ì‚Žü”g”‚̃}ƒCƒNƒ”g‚ɑ΂·‚éŽU—ŒvŽZ•û–@z—«‚³‚ñ‚ªR¸B

 

[PDF] researchgate.net

8[PDF] A generalized method for discriminating thermodynamic phase and retrieving cloud optical thickness and effective radius using transmitted shortwave radiance c

SE LeBlanc, P Pilewskie, KS Schmidtc - Meas. Tech c, 2014 - researchgate.net

c The instruments that pro- 15 vided data for this study were: pyranometer, pyrgeometer, ceilometer,
micro rain radar (MRR), sky webcam, and a spectral c On 6 August 2012, MRR measurements
of backscatter indicated the presence of a 
melting layer that was also present 1 h c

  Cited by 3 Related articles All 5 versions 

y96‚Æ“¯‚¶’˜ŽÒBzƒŠƒgƒŠ[ƒoƒ‹‚É‚æ‚éŒõŠw“IŒú‚³‚È‚Ç‚Ì„’è

 

[PDF] archives-ouvertes.fr

9Étude des précipitations en Antarctique par télédétection radar, mesures in-situ, et intercomparaison de modèles de climat

C Palerme - 2014 - hal.archives-ouvertes.fr

Page 1. LEtude des précipitations en Antarctique par télédétection radar, mesures
in-situ, et intercomparaison de mod`eles de climat Cyril Palerme To cite this version:
Cyril Palerme. Étude des précipitations en Antarctique par c

  Related articles All 8 versions

yz

 

[HTML] proquest.com

10[HTML] Spectral signatures in shortwave radiation measurements to derive cloud and aerosol properties

SE LeBlanc - 2014 - search.proquest.com

Spectral signatures in shortwave radiation measurements to derive cloud and aerosol properties.
Abstract. The amplitude and spectral shape of shortwave radiation are used to retrieve aerosol
and cloud properties from airborne and ground based measurements c

  Related articles All 4 versions

y96,98‚Ì’˜ŽÒ‚É‚æ‚éD˜_z‰_‚ƃGƒAƒƒ]ƒ‹‚Ì•úŽË“Á«‚ÌÄŒ»‚ÉŠÖ‚·‚錤‹†B