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Estimates of the Global Water Budget and Its Annual Cycle Using Observational and Model Data
by
Trenberth, Kevin E.
, Qian, Taotao
, Fasullo, John
, Smith, Lesley
, Dai, Aiguo
in
Atmospheric moisture
/ Atmospherics
/ Climate change
/ Climate cycles
/ Datasets
/ Evaporation
/ Global climate models
/ Oceans
/ Precipitation
/ SPECIAL SECTION: Global Energy and Water Cycle Experiment (GEWEX)
/ Water cycle
2007
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Estimates of the Global Water Budget and Its Annual Cycle Using Observational and Model Data
by
Trenberth, Kevin E.
, Qian, Taotao
, Fasullo, John
, Smith, Lesley
, Dai, Aiguo
in
Atmospheric moisture
/ Atmospherics
/ Climate change
/ Climate cycles
/ Datasets
/ Evaporation
/ Global climate models
/ Oceans
/ Precipitation
/ SPECIAL SECTION: Global Energy and Water Cycle Experiment (GEWEX)
/ Water cycle
2007
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Do you wish to request the book?
Estimates of the Global Water Budget and Its Annual Cycle Using Observational and Model Data
by
Trenberth, Kevin E.
, Qian, Taotao
, Fasullo, John
, Smith, Lesley
, Dai, Aiguo
in
Atmospheric moisture
/ Atmospherics
/ Climate change
/ Climate cycles
/ Datasets
/ Evaporation
/ Global climate models
/ Oceans
/ Precipitation
/ SPECIAL SECTION: Global Energy and Water Cycle Experiment (GEWEX)
/ Water cycle
2007
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Estimates of the Global Water Budget and Its Annual Cycle Using Observational and Model Data
Journal Article
Estimates of the Global Water Budget and Its Annual Cycle Using Observational and Model Data
2007
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Overview
A brief review is given of research in the Climate Analysis Section at NCAR on the water cycle. Results are used to provide a new estimate of the global hydrological cycle for long-term annual means that includes estimates of the main reservoirs of water as well as the flows of water among them. For precipitationPover land a comparison among three datasets enables uncertainties to be estimated. In addition, results are presented for the mean annual cycle of the atmospheric hydrological cycle based on 1979–2000 data. These include monthly estimates ofP, evapotranspirationE, atmospheric moisture convergence over land, and changes in atmospheric storage, for the major continental landmasses, zonal means over land, hemispheric land means, and global land means. The evapotranspiration is computed from the Community Land Model run with realistic atmospheric forcings, including precipitation that is constrained by observations for monthly means but with high-frequency information taken from atmospheric reanalyses. Results forE − Pare contrasted with those from atmospheric moisture budgets based on 40-yr ECMWF Re-Analysis (ERA-40) data. The latter show physically unrealistic results, because evaporation often exceeds precipitation over land, especially in the Tropics and subtropics.
Publisher
American Meteorological Society
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