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Meer Mohammed Ali, Neetu Singh, Manchikanti Suresh Kumar, Yangxing Zheng, Mark Bourassa, Chandra Mohan Kishtawal and Chandu Venkateswara Rao
The thermal energy needed for the development of hurricanes and monsoons as well as any prolonged marine weather event comes from layers in the upper oceans, not just from the thin layer represented by sea surface temperature alone. Ocean layers have dif...
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Weiqing Han, Detlef Stammer, Gerald A. Meehl, Aixue Hu, Frank Sienz and Lei Zhang
Previous studies suggest that anthropogenic warming has affected the multi-decadal trend patterns of sea level over the Indian Ocean (IO). This effect, however, has not been quantified. Using observational datasets combined with large ensemble experiment...
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Jingpeng Liu, Hong-Li Ren, Weijing Li and Jinqing Zuo
During the boreal summer from June to August, rainfall in Southwestern China shows substantial interdecadal variabilities on timescales longer than 10 years. Based on observational analyses and numerical modeling, we investigated the characteristics of i...
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Yun Liang, Yan Du, Lianyi Zhang, Xiaotong Zheng and Shuang Qiu
The Sea Surface Temperature (SST) in the South Tropical Indian Ocean (STIO) displays significant intraseasonal oscillation (ISO) in two regions. A striking 30?50-day ISO found over the east of thermocline ridge (Region A, 80?90° E, 6?12° S), as identifie...
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Seogyeong Kim, Kyung-Ja Ha, Ruiqiang Ding and Jiangping Li
This study examines the decadal change in the relationship between two major Indian Ocean (IO) sea surface temperature patterns, namely the Indian Ocean dipole (IOD) and northern IO and the East Asia summer monsoon (EASM) in the early 2000s. In 1991&ndas...
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