Multiforced statistical assessments of greenhouse-gas-induced surface air temperature change 1890–1985

1991 ◽  
Vol 6 (1) ◽  
pp. 23-33 ◽  
Author(s):  
Christian-D Schönwiese ◽  
Ursula Stähler
Author(s):  
Yu Wang ◽  
Pengcheng Yan ◽  
Fei Ji ◽  
Shankai Tang ◽  
Liu Yang ◽  
...  

2016 ◽  
Vol 129 (3-4) ◽  
pp. 1133-1144 ◽  
Author(s):  
Wei Hua ◽  
Samuel S. P. Shen ◽  
Alexander Weithmann ◽  
Huijun Wang

2010 ◽  
Vol 53 (2) ◽  
pp. 261-269 ◽  
Author(s):  
Xu-Chao YANG ◽  
Yi-Li ZHANG ◽  
Ming-Jun DING ◽  
Lin-Shan LIU ◽  
Zhao-Feng WANG ◽  
...  

2010 ◽  
Vol 1 (2) ◽  
pp. 84-90 ◽  
Author(s):  
Soikun Fong ◽  
Chisheng Wu ◽  
Anyu Wang ◽  
Xiajiang He ◽  
Ting Wang ◽  
...  

2009 ◽  
Vol 52 (8) ◽  
pp. 1207-1215 ◽  
Author(s):  
XuChao Yang ◽  
YiLi Zhang ◽  
LinShan Liu ◽  
Wei Zhang ◽  
MingJun Ding ◽  
...  

1978 ◽  
Vol 10 (2) ◽  
pp. 141-149 ◽  
Author(s):  
Larry D. Williams

It has been suggested that the Laurentide Ice Sheet originated with extensive perennial snow cover, and that the snow cover affected climate so as to aid ice-sheet development. In this study, a large increase in extent of October 1st snow cover in the Canadian Arctic from 1967–1970 to 1971–1975 is compared to changes in October means of other climate variables. Over the area of snow-cover expansion, mean surface air temperature decreased by up to 3°C, mean 500-mbar height was lowered by over 60 m, and precipitation was increased by up to a factor of two. These effects, if applied to the entire summer, together with the temperature change computed by Shaw and Donn for a Northern Hemisphere summer insolation minimum (the Milankovich effect), can account for glacierization of the Central Canadian Arctic.


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