A relationship between reflectivity and snow rate for a high-altitude s-band radar

Journal of Applied Meteorology and Climatology

Volumn 51, Issue 6, 2012, Pages 1111-1128

  Wolfe, Jonathan P ^a   Snider, Jefferson R ^b  

^a National Weather Service   (United States)

^b UNIVERSITY OF WYOMING   (United States)

Author keywords

Cloud microphysics; Cloud retrieval; Instrumentation sensors; Precipitation; Radars Radar observations

Indexed keywords

CLOUD MICROPHYSICS; CLOUD RETRIEVAL; DATA PAIRS; EMPIRICAL RELATIONSHIPS; EQUIVALENT REFLECTIVITY; HIGH ALTITUDE; HUMID AIR; ICE CRYSTALS; ICE NUCLEATION; INSTRUMENTATION/SENSORS; LOW LEVEL; PRECIPITATION INTENSITY; RADAR REFLECTIVITIES; RANGE GATES; ROCKY MOUNTAINS; S-BAND RADAR; SURFACE DETECTION; TEMPERATURE DEPENDENCE; UPSLOPE FLOWS; VERTICAL SEPARATION; WYOMING;

ATMOSPHERIC MOVEMENTS; CRYSTAL GROWTH; PRECIPITATION (CHEMICAL); REFLECTION; SNOW; TRACKING RADAR;

RADAR MEASUREMENT;

CLOUD MICROPHYSICS; CRYSTAL STRUCTURE; ICE CRYSTAL; PRECIPITATION INTENSITY; RADAR; REFLECTIVITY; SENSOR; SNOW; SNOWSTORM;

CHEYENNE; ROCKY MOUNTAINS; UNITED STATES; WYOMING;

EID: 84864995330     PISSN: 15588424     EISSN: 15588432     Source Type: Journal    
DOI: 10.1175/JAMC-D-11-0112.1     Document Type: Article

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