SK Das, M 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
CL Muller, A Baker, IJ Fairchildc - Journal of c, 2015 -
journals.ametsoc.org
c 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
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
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-14-0211.1j
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
L Wen, K Zhao, G Zhang, M 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
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 (melting) layer 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
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‰
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
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
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 (43‹38ŒN, 116‹42ŒE)j‚Å2‚‚̑wó«~…‚ðŠÏ‘ªBsequential intensity filtering technique (SIFT)‚È‚éƒtƒBƒ‹ƒ^ƒŠƒ“ƒO‚É‚æ‚Á‚ÄZRŠÖŒWŽ®‚ÌŒW”‚ª‚悇‚¤‚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
1Convective rain study with radiometer, radar and electric
field observations at a tropical location
A Maitra, S 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 Das, A 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
3Dependence of rain integral parameters on measured rain
drop velocities at a tropical location
T Sarkar, S Jana, A Maitra - URSI Asia-Pacific Radio
Science c, 2016 - ieeexplore.ieee.org
c 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 Sarkar, S Das, A 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
G Rakshit, A 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
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
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‚©‚甶‚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
T Sarkar, S Das, A Maitra - Atmospheric Research, 2015 -
Elsevier
c 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
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
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
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
y~MRR‚ð—p‚¢‚½~…ƒ^ƒCƒv‚Ì•ª—Þz
G Rakshit, R 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
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
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
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
JM Erlingis, JJ Gourley, PE 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‚鋧㸂ª‘Η¬‚ðˆÛŽ‚µA’†‰›—±Œa‚Ì‘å‚«‚È~…—±Œa•ª•z‚Æ‚È‚éB
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
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
K Friedrich, EA 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
A Maitra, S Jana, R 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
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
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
BK Guha, R Chakraborty, B Nandyc - c and
Devices for c, 2015 - ieeexplore.ieee.org
c 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
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
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
y¢BB‚Ì‹CŒó’l‚ðáü‚Ì”»’f‚É—˜—pzTRMM-PR‚ð—p‚¢‚½BB‚Ì”»’èB‚•W‚•”‚Å‚ÌŠÏ‘ª‚ð—p‚¢‚ÄŒŸØB
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
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
G Rakshit, A 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^
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
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‚¨‚»‚炃uƒ‰ƒCƒgƒoƒ“ƒhŒŸoiNBB~…‚Ì’Šoj‚É—˜—pz
M Frech, M Hagen, T
Mammen - Journal of Atmospheric and c, 2017 - journals.ametsoc.org
c This is verified
using a Micro 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
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
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
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
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
R Chakraborty, S Talukdar, U Saha, S 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
N Mazari, HO Sharif, H 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
MR Kumjian, KA 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
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
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‚͂悈ê’v‚µ‚½B
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
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
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
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
D Gochis, R Schumacher, K Friedrichc - Bulletin of the c,
2015 - journals.ametsoc.org
Cited by 89 Related articles All 11 versions
yz
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
R Chakraborty, S Talukdar, U Saha, S 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
N Mazari, HO Sharif, H 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
MR Kumjian, KA 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
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
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
yŽR’n•”‚É‚¨‚¯‚é~á‰_‚Ì“Á’¥z
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
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
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
D Gochis, R Schumacher, K Friedrichc - Bulletin of the c,
2015 - journals.ametsoc.org
Cited by 89 Related articles All 11 versions
yz
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
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
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
T Iguchi, T Matsui, WK Tao, AP 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
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
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
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
y—Z‰ð‘w‚ðŠÜ‚Þ~…‚̉”’¼•ª•z‚Ì“Á’¥z
S Das, A 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
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
y63‚Æ“¯“à—eBWRF-SBMiƒXƒyƒNƒgƒ‹ƒrƒ“ƒ‚ƒfƒ‹G~áŽí‚Í6ŒÂjz
M Konwar, SK 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
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
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
SK Das, SM Deshpande, SS Das, M 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
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
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
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
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
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
TH Raupach, A 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
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
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
y¢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
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
I
Rahayu, M Marzuki, H 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
M Arulraj, AP 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
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
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
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
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
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
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 micro- rain 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
4Weather
observations on Whistler Mountain during five storms
2014 -
Springer JM Thériault, KL 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
a 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
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
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
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
y~WillieŽ‚ÌD˜_z•¡”‚̃Œ[ƒ_‚ð—p‚¢‚ÄŽÕ•Áˆæ‚̸“x‚ð‚‚ß‚éB
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
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
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
1구름씨뿌리기에 의한 구름 및 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
yz
2산악 지형에서의 지상기반 빙정핵 시딩효과 검증을 위한 MRR 및 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
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
y~zƒ{ƒ‹ƒOˆæ‚Ì“ú~…—ʂ͂قڑΗ¬«‚Ì~…‚É‚æ‚é‚à‚Ì‚Å‚ ‚Á‚½B
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
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
yÚ‘±•s‰Âz
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
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
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
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
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