Contributions of the Liquid and Ice Phases to Global Surface Precipitation: Observations and Global Climate Modeling
This study is the first to reach a global view of the precipitation process partitioning, using a combination of satellite and global climate modeling data. The pathways investigated are (1) precipitating ice (ice/snow/graupel) that forms above the freezing level and melts to produce rain (S) followed by additional condensation and collection as the melted precipitating ice falls to the surface (R); (2) growth completely through condensation and collection (coalescence), warm rain (W); and (3) precipitating ice (primarily snow) that falls to the surface (SS). To quantify the amounts, data from satellite-based radar measurementsâCloudSat, GPM, and TRMMâare used, as well as climate model simulations from the Community Atmosphere Model (CAM) and the UK Met Office Unified Model (UM).
dataset
https://gdex.ucar.edu/dataset/id/93bf94ea-38b7-4d72-a4cb-8a9a8d4091fd.html
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name: Contributions of the Liquid and Ice Phases to Global Surface Precipitation: Observations and Global Climate Modeling
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Dataset
revision
2014-10-16
EARTH SCIENCE > ATMOSPHERE > PRECIPITATION > LIQUID PRECIPITATION > RAIN
EARTH SCIENCE > ATMOSPHERE > PRECIPITATION > PRECIPITATION RATE
EARTH SCIENCE > ATMOSPHERE > PRECIPITATION > SOLID PRECIPITATION
EARTH SCIENCE > ATMOSPHERE > PRECIPITATION > SOLID PRECIPITATION > SNOW
EARTH SCIENCE > ATMOSPHERE > PRECIPITATION > TOTAL SURFACE PRECIPITATION RATE
revision
2018-03-15
-180.0
180.0
90.0
-90.0
publication
2020-04-10
modified
2020-03-20
application/x-tika-ooxml
Creative Commons Attribution 4.0 International License.
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UCAR/NCAR - Mesoscale and Microscale Meteorology Laboratory
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UCAR/NCAR - GDEX
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2022-07-21T12:31:13-06:00