download

More documents

Recommendations

Info

Regional‐scale surface temperature evolutions The warming signal has emerged rather monotonically in the Indian Ocean/western Pacific region during the past century. The tropical eastern Pacific、North Pacific and North Atlantic are regions where the warming signal appears to emerge from a background of more substantial multidecadal variability.
Contributions of natural and anthropogenic forcings —expressed by ratio of explainable variance Globalland Globalocean Northern extratropics Southern extratropics Indian Ocean/Western Pacific Warm Pool Tropical Eastern Pacific N. Pacific N. Atlantic NAT 7.4% 1.6% 27.3% 26.1% 1.1% 0.4% 8.0% 18.9% Athro 76.6% 70.2% 61.5% 48.0% 76.7% 41.1% 47.2% 6.5% For land and hemispheric means, external forcings could explain most of the variance. Contributions from internal variability are larger than from external forcings in the tropical eastern Pacific and North Atlantic region . 13
Page 1 and 2: Contributions of Natural and Anthro
Page 3 and 4: Background • A project entitled
Page 5 and 6: Framework of FGOALS_gl 1*1 L30 LICO
Page 7 and 8: Global annual mean temperature seri
Page 9 and 10: Surface temperature trends over the
Page 11: Land‐ and hemispheric‐ scale su
Page 15 and 16: Observed and simulated surface temp
Page 17: Conclusions 1) The simulations supp
Page 20: Global average SAT in CMIP3 Models

download

Create successful ePaper yourself

Delete template?

Save as template?