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Title: Validation of a Statistical Methodology for Extracting Vegetation Feedbacks: Focus on North African Ecosystems in the Community Earth System Model

Journal Article · · Journal of Climate
 [1];  [2];  [2];  [3];  [3];  [3]
  1. Nelson Institute Center for Climatic Research, University of Wisconsin–Madison, Madison, Wisconsin, and Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California
  2. Nelson Institute Center for Climatic Research, University of Wisconsin–Madison, Madison, Wisconsin
  3. Environmental Sciences Division, and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, Tennessee

Generalized equilibrium feedback assessment (GEFA) is a potentially valuable multivariate statistical tool for extracting vegetation feedbacks to the atmosphere in either observations or coupled Earth system models. The reliability of GEFA at capturing the terrestrial impacts on regional climate is demonstrated in this paper using the National Center for Atmospheric Research Community Earth System Model (CESM), with focus on North Africa. The feedback is assessed statistically by applying GEFA to output from a fully coupled control run. To reduce the sampling error caused by short data records, the traditional or full GEFA is refined through stepwise GEFA by dropping unimportant forcings. Two ensembles of dynamical experiments are developed for the Sahel or West African monsoon region against which GEFA-based vegetation feedbacks are evaluated. In these dynamical experiments, regional leaf area index (LAI) is modified either alone or in conjunction with soil moisture, with the latter runs motivated by strong regional soil moisture–LAI coupling. Stepwise GEFA boasts higher consistency between statistically and dynamically assessed atmospheric responses to land surface anomalies than full GEFA, especially with short data records. GEFA-based atmospheric responses are more consistent with the coupled soil moisture–LAI experiments, indicating that GEFA is assessing the combined impacts of coupled vegetation and soil moisture. Finally, both the statistical and dynamical assessments reveal a negative vegetation–rainfall feedback in the Sahel associated with an atmospheric stability mechanism in CESM versus a weaker positive feedback in the West African monsoon region associated with a moisture recycling mechanism in CESM.

Research Organization:
Univ. of Wisconsin, Madison, WI (United States); Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER); National Science Foundation (NSF)
Grant/Contract Number:
SC0012534; AC05-00OR22725; AGS-1343904
OSTI ID:
1419613
Alternate ID(s):
OSTI ID: 1422596
Journal Information:
Journal of Climate, Journal Name: Journal of Climate Vol. 31 Journal Issue: 4; ISSN 0894-8755
Publisher:
American Meteorological SocietyCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 12 works
Citation information provided by
Web of Science

Cited By (4)

Elucidating observed land surface feedbacks across sub-Saharan Africa journal March 2019
Observed land surface feedbacks on the Australian monsoon system journal February 2020
Influence of Central Siberian Snow‐Albedo Feedback on the Spring East Asian Dust Cycle and Connection With the Preceding Winter Arctic Oscillation journal December 2018
Climatology of Asian dust activation and transport potential based on MISR satellite observations and trajectory analysis journal January 2019