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Climate‐vegetation interaction and amplification of Australian dust variability
Author(s) -
Evans Stuart,
Ginoux Paul,
Malyshev Sergey,
Shevliakova Elena
Publication year - 2016
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2016gl071016
Subject(s) - vegetation (pathology) , environmental science , forcing (mathematics) , atmospheric sciences , snow , precipitation , atmosphere (unit) , climatology , radiative forcing , mineral dust , atmospheric dust , climate model , radiative transfer , geology , climate change , meteorology , aerosol , oceanography , geography , geomorphology , physics , medicine , pathology , quantum mechanics
Abstract Observations show that Australian dust activity varies by a factor of 4 on decadal timescales. General circulation models, however, typically fail to simulate this variability. Here we introduce a new dust parameterization into the NOAA/Geophysical Fluid Dynamics Laboratory climate model CM3 that represents land surface processes controlling dust sources including soil water and ice, snow cover, vegetation characteristics, and land type. In an additional novel step, we couple this new dust parameterization to the dynamic vegetation model LM3. In Australia, the new parameterization amplifies the magnitude and timescale of dust variability and better simulates the El Niño–Southern Oscillation‐dust relationship by more than doubling its strength. We attribute these improvements primarily to the slow response time of vegetation to precipitation anomalies and show that vegetation changes account for approximately 50% of enhanced dust emission during El Niño events. The amplified dust leads to radiative forcing over Australia greater than −1 and −20 W/m 2 at top of atmosphere and surface, respectively.