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- W3146088178 abstract "借助于通过 sedimentological， biogeological 和 geomorphologic 数据的编译的文学的调查，内陆湖水平在 6 和 18 ka B. P 在干旱或半干旱的大陆亚洲变化。被重建了。结果证明从西方、西北的亚洲的湖被描绘由很，高水位线在 18 ka B.P. 铺平，但是低或中间的水站在 6 ka B. P。因此，在这个区域的高湖水平与 westerlies 的向南方的排水量被联系高湖看台的程度在冻结成冰期间显示了 westerlies 的南部的胁腹。相反地，从东方、南部的亚洲的湖在 18 ka B. P 登记了比较底层。并且在 6 ka B. P 的显著地高的。在 18 ka B. P 降低湖水平。被削弱的夏天季风和高湖水平在 6 ka B. P 引起。由在土地和海洋之间的扩大热对比导致的提高的夏天季风。高湖层次的程度显示了季风扩大的北边界。在上述二个区域之间，在湖行为在 6 ka B. P 在东南的亚洲接近了那的中亚有一个气候的过渡地区。但是在 18 ka B. P 在西北的亚洲变得类似于那。因此，这个地区从季风成为了一个过渡部门到 westerlies。" @default.
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- W3146088178 date "1998-01-01" @default.
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- W3146088178 title "The reconstruction and interpretations of lake status at 6 ka and 18 ka B.P.in inland mainland Asia" @default.
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