%0 Journal Article
%T DYNAMICS OF LATERAL BOUNDARY MESO-SCALE JET IN THE OCEAN AND ATMOSPHERE<br>
%A Chao Jiping
%A <br>
%J 大气科学进展
%D 1984
%I 
%X By using an ageostrophie shallow water model, it is pointed out that a kind of lateral boundary meso-seales jet can be established near the plateau or coast. The charactcristie width of this kind of jet is proportional to the scale of Lc = L(?)C(?)(?),where Lo= Cof is the radius of Rossby deformation, Co= (y*H)the speed of gravity wave and g* the redueced gravity. In general, L(?) is of the order of one hundred kilometers and lens of kilometers in the atmosphere and in the ocean respectively. The large-scale gcostrophic current is an important background condition for forming this kind of jet. From this view point it seems that this kind of atmospheric meso-scale jet only occurs in late spring and summer in the eastern part of Asia, because there is a large-scale south monsoon over there. For the ocean, this kind of meso-scale jct seems to be a semi-persistant syslem and not to show a signilieanl seasonal variation, and it can be established on both sides of the ocean.
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=28A2F569B2458C17&jid=5434AFBF6CB6E7E8D67733B541F211C7&aid=B8246F338BF2FCCB5F02FBFAC483E25E&yid=36250D1D6BDC99BD&vid=CA4FD0336C81A37A&iid=0B39A22176CE99FB&sid=FCD27DC5E1F2EEE7&eid=EF27C460877D3C9F&journal_id=0256-1530&journal_name=大气科学进展&referenced_num=0&reference_num=0