ASCAT observations of downdrafts from mesoscale convective systems
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[1] Brian E. Mapes,et al. Composite Life Cycle of Maritime Tropical Mesoscale Convective Systems in Scatterometer and Microwave Satellite Observations , 2009 .
[2] Wenming Lin,et al. ASCAT Wind Quality Control Near Rain , 2015, IEEE Transactions on Geoscience and Remote Sensing.
[3] R. Houze. Mesoscale convective systems , 2004 .
[4] Wenming Lin,et al. Rain Identification in ASCAT Winds Using Singularity Analysis , 2014, IEEE Geoscience and Remote Sensing Letters.
[5] M. Katsumata,et al. Variability in surface meteorology and air‐sea fluxes due to cumulus convective systems observed during CINDY/DYNAMO , 2014 .
[6] Wenming Lin,et al. Rain Effects on ASCAT-Retrieved Winds: Toward an Improved Quality Control , 2012, IEEE Transactions on Geoscience and Remote Sensing.
[7] S. Milton,et al. The impact of convective cold pool outflows on model biases in the Sahara , 2013 .
[8] S. Rutledge,et al. Surface Fluxes and Boundary Layer Recovery in TOGA COARE: Sensitivity to Convective Organization , 1998 .
[9] G. Young,et al. Convective Wakes in the Equatorial Western Pacific during TOGA , 1995 .
[10] R. Carbone,et al. Excitation of rainfall over the Tropical Western Pacific , 2012 .
[11] R. J. Reed,et al. Diurnal Variations in Convective Activity and Precipitation During Phases II and III of GATE , 1978 .
[12] Edward J. Zipser,et al. Mesoscale and convective-scale downdrafts as distinct components of squall-line structure , 1977 .
[13] S. P. Anderson,et al. Surface meteorology and air-sea fluxes in the western equatorial Pacific warm pool during the TOGA c , 1996 .
[14] Richard H. Johnson,et al. A Composite Analysis of the Boundary Layer Accompanying a Tropical Squall Line , 1983 .
[15] Marcos Portabella,et al. Rain Detection and Quality Control of SeaWinds , 2001 .
[16] G. Kiladis,et al. Squall Lines and Convectively Coupled Gravity Waves in the Tropics: Why Do Most Cloud Systems Propagate Westward? , 2012 .
[17] Robert A. Houze,et al. Structure and Dynamics of a Tropical Squall–Line System , 1977 .
[18] M. Drinkwater,et al. The advanced scatterometer (ASCAT) on the meteorological operational (MetOp) platform: A follow on for European wind scatterometers , 2002 .
[19] Yukari N. Takayabu,et al. Large-Scale Cloud Disturbances Associated with Equatorial Waves: Part II: Westward-Propagating Inertio-Gravity Waves@@@Part II 西進慣性重力波 , 1994 .
[20] Yukari N. Takayabu,et al. Observation of a quasi-2-day wave during TOGA COARE , 1996 .
[21] M. Garstang,et al. Downdrafts from tropical oceanic cumuli , 1984 .
[22] Jean Tournadre,et al. Impact of rain cell on scatterometer data: 1. Theory and modeling , 2003 .
[23] J. Gamache,et al. Mesoscale Air Motions Associated with a Tropical Squall Line , 1982 .
[24] S. Hristova-Veleva,et al. Challenges to Satellite Sensors of Ocean Winds: Addressing Precipitation Effects , 2012 .
[25] D. Chelton,et al. Covariability of Surface Wind and Stress Responses to Sea Surface Temperature Fronts , 2012 .
[26] Hiroaki Miura,et al. Diurnal Cycle of Precipitation in the Tropics Simulated in a Global Cloud-Resolving Model , 2009 .
[27] P. Zuidema,et al. Simulated Convective Invigoration Processes at Trade Wind Cumulus Cold Pool Boundaries , 2014 .
[28] C. Kummerow,et al. A Multisensor Observational Depiction of the Transition from Light to Heavy Rainfall on Subdaily Time Scales , 2013 .
[29] Jean Tournadre,et al. Impact of rain cell on scatterometer data: 2. Correction of Seawinds measured backscatter and wind and rain flagging , 2005 .
[30] Bertrand Chapron,et al. Compatibility of C- and Ku-band scatterometer winds: ERS-2 and QuikSCAT , 2013 .