Next Article in Journal
Understanding the Variability of West African Summer Monsoon Rainfall: Contrasting Tropospheric Features and Monsoon Index
Previous Article in Journal
Evaluation of Meteorological Drought and Flood Scenarios over Kenya, East Africa
Open AccessArticle

Global Dimming and Brightening Features during the First Decade of the 21st Century

1
Laboratory of Meteorology, Department of Physics, University of Ioannina, 45110 Ioannina, Greece
2
LATMOS/IPSL, Sorbonne Université, UVSQ, CNRS, 75252 Paris, France
3
Department of Environment, University of the Aegean, 81100 Mytilene, Greece
4
R & D Satellite Observations Department, Royal Netherlands Meteorological Institute (KNMI), 3730 AE De Bilt, The Netherlands
5
Department of Environmental Engineering, University of Patras, 74148 Agrinio, Greece
6
Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland
7
Department of Physics, University of Crete, 71003 Heraklion, Crete, Greece
*
Author to whom correspondence should be addressed.
Atmosphere 2020, 11(3), 308; https://doi.org/10.3390/atmos11030308
Received: 27 January 2020 / Revised: 17 March 2020 / Accepted: 19 March 2020 / Published: 21 March 2020
(This article belongs to the Section Climatology)
Downward surface solar radiation (SSR) trends for the first decade of the 2000s were computed using a radiative transfer model and satellite and reanalysis input data and were validated against measurements from the reference global station networks Global Energy Balance Archive (GEBA) and Baseline Surface Radiation Network (BSRN). Under all-sky conditions, in spite of a somewhat patchy structure of global dimming and brightening (GDB), an overall dimming was found that is weaker in the Northern than in the Southern Hemisphere (−2.2 and −3.1 W m−2, respectively, over the 2001–2009 period). Dimming is observed over both land and ocean in the two hemispheres, but it is more remarkable over land areas of the Southern Hemisphere. The post-2000 dimming is found to have been primarily caused by clouds, and secondarily by aerosols, with total cloud cover contributing −1.4 W m−2 and aerosol optical thickness −0.7 W m−2 to the global average dimming of −2.65 W m−2. The evaluation of the model-computed GDB against BSRN and GEBA measurements indicates a good agreement, with the same trends for 65% and 64% of the examined stations, respectively. The obtained model results are in line with other studies for specific world regions and confirm the occurrence of an overall solar dimming over the globe during the first decade of 21st century. This post-2000 dimming has succeeded the global brightening observed in the 1990s and points to possible impacts on the ongoing global warming and climate change. View Full-Text
Keywords: surface solar radiation; climate; dimming; brightening; model; stations; satellite data surface solar radiation; climate; dimming; brightening; model; stations; satellite data
Show Figures

Figure 1

MDPI and ACS Style

Hatzianastassiou, N.; Ioannidis, E.; Korras-Carraca, M.-B.; Gavrouzou, M.; Papadimas, C.D.; Matsoukas, C.; Benas, N.; Fotiadi, A.; Wild, M.; Vardavas, I. Global Dimming and Brightening Features during the First Decade of the 21st Century. Atmosphere 2020, 11, 308.

Show more citation formats Show less citations formats
Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Article Access Map by Country/Region

1
Back to TopTop