Dynamical response of Mediterranean precipitation to greenhouse gases and aerosols

被引:36
作者
Tang, Tao [1 ]
Shindell, Drew [1 ]
Samset, Bjorn H. [2 ]
Boucher, Olivier [3 ]
Forster, Piers M. [4 ]
Hodnebrog, Oivind [2 ]
Myhre, Gunnar [2 ]
Sillmann, Jana [2 ]
Voulgarakis, Apostolos [5 ]
Andrews, Timothy [6 ]
Faluvegi, Gregory [7 ,8 ]
Flaschner, Dagmar [9 ]
Iversen, Trond [10 ]
Kasoar, Matthew [5 ]
Kharin, Viatcheslav [11 ]
Kirkevag, Alf [10 ]
Lamarque, Jean-Francois [12 ]
Olivie, Dirk [10 ]
Richardson, Thomas [4 ]
Stjern, Camilla W. [2 ]
Takemura, Toshihiko [13 ]
机构
[1] Duke Univ, Nicholas Sch Environm, Durham, NC 27706 USA
[2] CICERO Ctr Int Climate & Environm Res, Oslo, Norway
[3] Univ Paris 06, CNRS, Inst Pierre Simon Laplace, Paris, France
[4] Univ Leeds, Leeds, W Yorkshire, England
[5] Imperial Coll London, London, England
[6] Met Off Hadley Ctr, Exeter, Devon, England
[7] Columbia Univ, New York, NY USA
[8] NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[9] Max Planck Inst Meteorol, Hamburg, Germany
[10] Norwegian Meteorol Inst, Oslo, Norway
[11] Canadian Ctr Climate Modelling & Anal, Victoria, BC, Canada
[12] Natl Ctr Atmospher Res, Boulder, CO USA
[13] Kyushu Univ, Fukuoka, Fukuoka, Japan
基金
美国国家科学基金会;
关键词
EARTH SYSTEM MODEL; BLACK CARBON AEROSOLS; CLIMATE RESPONSE; VARIABILITY; SIMULATION; ATMOSPHERE; RADIATION; PDRMIP; CMIP5; LAND;
D O I
10.5194/acp-18-8439-2018
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Atmospheric aerosols and greenhouse gases affect cloud properties, radiative balance and, thus, the hydrological cycle. Observations show that precipitation has decreased in the Mediterranean since the beginning of the 20th century, and many studies have investigated possible mechanisms. So far, however, the effects of aerosol forcing on Mediterranean precipitation remain largely unknown. Here we compare the modeled dynamical response of Mediterranean precipitation to individual forcing agents in a set of global climate models (GCMs). Our analyses show that both greenhouse gases and aerosols can cause drying in the Mediterranean and that precipitation is more sensitive to black carbon (BC) forcing than to well-mixed greenhouse gases (WMGHGs) or sulfate aerosol. In addition to local heating, BC appears to reduce precipitation by causing an enhanced positive sea level pressure (SLP) pattern similar to the North Atlantic Oscillation Arctic Oscillation, characterized by higher SLP at midlatitudes and lower SLP at high latitudes. WMGHGs cause a similar SLP change, and both are associated with a northward diversion of the jet stream and storm tracks, reducing precipitation in the Mediterranean while increasing precipitation in northern Europe. Though the applied forcings were much larger, if forcings are scaled to those of the historical period of 1901-2010, roughly one-third (31 +/- 17 %) of the precipitation decrease would be attributable to global BC forcing with the remainder largely attributable to WMGHGs, whereas global scattering sulfate aerosols would have negligible impacts. Aerosol-cloud interactions appear to have minimal impacts on Mediterranean precipitation in these models, at least in part because many simulations did not fully include such processes; these merit further study. The findings from this study suggest that future BC and WMGHG emissions may significantly affect regional water resources, agricultural practices, ecosystems and the economy in the Mediterranean region.
引用
收藏
页码:8439 / 8452
页数:14
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