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Title: CAUSES: On the Role of Surface Energy Budget Errors to the Warm Surface Air Temperature Error Over the Central United States

Journal Article · · Journal of Geophysical Research: Atmospheres
DOI:https://doi.org/10.1002/2017JD027194· OSTI ID:1439003
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  1. Lawrence Livermore National Laboratory, Livermore CA USA
  2. Met Office, Exeter UK
  3. European Centre for Medium-Range Weather Forecasts, Reading UK
  4. Pacific Northwest National Laboratory, Richland WA USA
  5. Laboratoire de Météorologie Dynamique, Paris France
  6. Canadian Centre for Climate Modelling and Analysis, Environment Canada, Victoria British Columbia Canada
  7. CNRM, Meteo-France/CNRS, Toulouse France
  8. Research Center for Environmental Change, Academia Sinica, Taipei Taiwan

Many weather forecasting and climate models simulate a warm surface air temperature (T2m) bias over mid-latitude continents during the summertime, especially over the Great Plains. We present here one of a series of papers from a multi-model intercomparison project (CAUSES: Cloud Above the United States and Errors at the Surface), which aims to evaluate the role of cloud, radiation, and precipitation biases in contributing to T2m bias using a short-term hindcast approach with observations mainly from the Atmospheric Radiation Measurement (ARM) Southern Great Plains (SGP) site during the period of April to August 2011. The present study examines the contribution of surface energy budget errors to the bias. All participating models simulate higher net shortwave and longwave radiative fluxes at the surface but there is no consistency on signs of biases in latent and sensible heat fluxes over the Central U.S. and ARM SGP. Nevertheless, biases in net shortwave and downward longwave fluxes, as well as surface evaporative fraction (EF) are the main contributors to T2m bias. Radiation biases are largely affected by cloud simulations, while EF is affected by soil moisture modulated by seasonal accumulated precipitation and evaporation. An approximate equation is derived to further quantify the magnitudes of radiation and EF contributions to T2m bias. Our analysis suggests that radiation errors are always an important source of T2m error for long-term climate runs with EF errors either of equal or lesser importance. However, for the short-term hindcasts, EF errors are more important provided a model has a substantial EF bias.

Research Organization:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC05-76RL01830
OSTI ID:
1439003
Report Number(s):
PNNL-SA-126060; KP1701000
Journal Information:
Journal of Geophysical Research: Atmospheres, Vol. 123, Issue 5; ISSN 2169-897X
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English

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Cited By (9)

Improved Spatiotemporal Representativeness and Bias Reduction of Satellite‐Based Evapotranspiration Retrievals via Use of In Situ Meteorology and Constrained Canopy Surface Resistance journal February 2019
Reducing climate model biases by exploring parameter space with large ensembles of climate model simulations and statistical emulation journal January 2019
The Summertime Precipitation Bias in E3SM Atmosphere Model Version 1 over the Central United States journal August 2019
Surface Flux Equilibrium Theory Explains an Empirical Estimate of Water‐Limited Daily Evapotranspiration journal July 2019
Introduction to CAUSES: Description of Weather and Climate Models and Their Near‐Surface Temperature Errors in 5 day Hindcasts Near the Southern Great Plains journal March 2018
An Overview of the Atmospheric Component of the Energy Exascale Earth System Model journal August 2019
CAUSES: Diagnosis of the Summertime Warm Bias in CMIP5 Climate Models at the ARM Southern Great Plains Site journal March 2018
Satellite-based soil moisture provides missing link between summertime precipitation and surface temperature biases in CMIP5 simulations over conterminous United States journal February 2019
Regionally refined test bed in E3SM atmosphere model version 1 (EAMv1) and applications for high-resolution modeling journal January 2019

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