ON August 21,1998,the first women’s teamattempting to float down from the source of theChangjiang River started from Chengdu,SichuanProvince.We drove towards the west and traversed theSongpan grassland,going deep int...ON August 21,1998,the first women’s teamattempting to float down from the source of theChangjiang River started from Chengdu,SichuanProvince.We drove towards the west and traversed theSongpan grassland,going deep into the Qinghai-TibetanPlateau along the Zoige,Xining and Golmud routes.OnSeptember 11,we arrived at the source of the ChangjiangRiver-the foot of the snow-covered GeladaindongMountain.On September 26,all members of the team,traveling either by land or by water,safely assembled bythe Tuotuo River.展开更多
Some observational characteristics of residual current and mass transport in the Hangzhou Bay and the Changjiang Estuary in winter are analyzed. The residual current and its impact on mass transport are simulated with...Some observational characteristics of residual current and mass transport in the Hangzhou Bay and the Changjiang Estuary in winter are analyzed. The residual current and its impact on mass transport are simulated with a 3 - D joint model for the Hangzhou Bay and the Changjiang Estuary, in which the impacts of river flux, wind, baroclinic pressure gradient (BPG), background current in the East China Sea and tide (including M2, S2, K1 and O1) are taken into account. Based on there studies, further simulations are made to analyze the dynamical mechanisms of the observational characteristics.展开更多
文摘ON August 21,1998,the first women’s teamattempting to float down from the source of theChangjiang River started from Chengdu,SichuanProvince.We drove towards the west and traversed theSongpan grassland,going deep into the Qinghai-TibetanPlateau along the Zoige,Xining and Golmud routes.OnSeptember 11,we arrived at the source of the ChangjiangRiver-the foot of the snow-covered GeladaindongMountain.On September 26,all members of the team,traveling either by land or by water,safely assembled bythe Tuotuo River.
基金the Major Stste Basic Research Program Under contract Grand No. G1999043803, theNational Natural Science Foundation of China u
文摘Some observational characteristics of residual current and mass transport in the Hangzhou Bay and the Changjiang Estuary in winter are analyzed. The residual current and its impact on mass transport are simulated with a 3 - D joint model for the Hangzhou Bay and the Changjiang Estuary, in which the impacts of river flux, wind, baroclinic pressure gradient (BPG), background current in the East China Sea and tide (including M2, S2, K1 and O1) are taken into account. Based on there studies, further simulations are made to analyze the dynamical mechanisms of the observational characteristics.
