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Pollution trends over Europe constrain global aerosol forcing as simulated by climate models
Author(s) -
Cherian Ribu,
Quaas Johannes,
Salzmann Marc,
Wild Martin
Publication year - 2014
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 - 10.1002/2013gl058715
Subject(s) - forcing (mathematics) , aerosol , radiative forcing , environmental science , atmospheric sciences , climatology , cloud forcing , climate model , sky , pollution , cloud cover , meteorology , climate change , cloud computing , physics , geology , ecology , oceanography , biology , computer science , operating system
An increasing trend in surface solar radiation (solar brightening) has been observed over Europe since the 1990s, linked to economic developments and air pollution regulations and their direct as well as cloud‐mediated effects on radiation. Here, we find that the all‐sky solar brightening trend (1990–2005) over Europe from seven out of eight models (historical simulations in the Fifth Coupled Model Intercomparison Project) scales well with the regional and global mean effective forcing by anthropogenic aerosols (idealized “present‐day” minus “preindustrial” runs). The reason for this relationship is that models that simulate stronger forcing efficiencies and stronger radiative effects by aerosol‐cloud interactions show both a stronger aerosol forcing and a stronger solar brightening. The all‐sky solar brightening is the observable from measurements (4.06±0.60 W m −2 decade −1 ), which then allows to infer a global mean total aerosol effective forcing at about −1.30 W m −2 with standard deviation ±0.40 W m −2 .