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| 1 | From MONEX to the Global Monsoon:A Review of Monsoon System Research显示文摘Substantial progress has been made over the past three decades since the Monsoon Experiments(MONEX) of 1978–79. Here, we review these achievements by highlighting four breakthroughs in monsoon research:(1) The identification of the coupled ocean–land–atmosphere nature of the monsoon in the process of the annual cycle of solar heating;(2) new understanding of the changes in the driving forces of monsoon systems, with anthropogenic factors(climate effects of increased greenhouse gas and aerosol emissions) playing an important role in the regulation of monsoons;(3) detection of the interdecadal- and centennial-scale variability of monsoon systems, and its attribution to the combined impact of global warming and natural(especially oceanic) effects; and(4) the emerging concept of the global monsoon and its long-term variation under the impact of global climate change. All the observational and model-derived evidence demonstrates that the monsoon system, as an important component of the global climate system, has already changed and will continue to change in the future. This picture of an evolving monsoon system poses great challenges for near-term prediction and long-term projection. | DING Yihui LIU Yanju SONG Yafang ZHANG Jin | 2015 | Advances in Atmospheric Sciences2015，32，1： | 14 |
| 2 | Decadal change of the East Asian summer monsoon and its related surface temperature in Asia-Pacific during 1880–2004显示文摘The East Asian summer monsoon(EASM)and its related change of surface temperature in the past century were not clearly addressed due to absence of atmospheric reanalysis data before 1948.On the benchmark of station-observed sea level pressure(SLP)in China,we utilized multiple SLP datasets and evaluated their qualities in measuring the SLP-based EASM index(EASMI).It is found that the EASMI based on the SLP of the Hadley center version 2(HadSLP2)has shown the best performance on the interannual and decadal time scales.Instead of showing a linear weakening trend pointed out by the previous study,the EASMI has likely exhibited the decadal variability,characterized by weakened trends during 1880–1906,1921–1936,and 1960–2004,and with enhanced trends during 1906–1921 and 1936–1960,respectively.Corresponding to the weakened and enhanced periods of EASMI since the 1920s,the surface air temperature(SAT)index(SATI)averaged in eastern China has likely shown a warming and a cooling trend,respectively.However,the decadal abrupt transitions between the two indices do not occur concurrently,which results in a weak correlation between two indices on the decadal time scale.Further analysis indicates that there are four key regions where the SAT is significantly correlated with the EASMI,suggesting the joint impact of surface temperature in Asia-Pacific on the EASM during 1880–2004.In which,the decadal change of SAT near the Lake Baikal plays an important role in the linear trends of the EASM before and after 1960. | LIN Xiang ZHU CongWen Lü JunMei | 2013 | Chinese Science Bulletin2013，58，35： | 2 |
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