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采用1947—1965年每2°网格点上月平均气候资料计算20°S以北的太平洋洋面上热量交换。本文给出了比其它作者的图更细致并更紧密地与气候区域相联系地热量交换的各个分量图。总热量交换的积分指出北太平洋大约以3×10~(14)卡/秒速率获得热量,这也许是北大洋盆地中没有深水形成的原因之一。这热量获得是由平均速度为1.25×10~(-5)厘米/秒的深水上升所抵偿。北太平洋海水的平衡是由流量为8百万米~3/秒的暖表层水的外流来维持的,这暖流一部分经过印度尼西亚水域,一部分在热带太平洋东部从赤道逆流流到南赤道洋流。北太平洋获得热量的地方主要是在其东沿和25°N以南的地区,主要的热量损耗发生在黑潮地区。在这些热源和热汇存在的情况下,付热带反气旋范围内平均温度的分布,由大约为10百万米~3/秒流量的表层浅水的水平环流来维持。
Calculate the heat exchange over the Pacific Ocean north of 20 ° S using the monthly mean climatological data of 2 ° grid points from 1947 to 1965. This paper presents various components of heat exchange that relate more closely and closely to climate regions than other authors’ diagrams. The points for total heat exchange indicate that the North Pacific receives heat at a rate of about 3 × 10 ~ (14) kcal / sec, which may be one of the reasons for the absence of deep water in the northern ocean basin. This heat gain is offset by a deepwater rise of 1.25 x 10 ~ (-5) cm / sec average speed. The balance of the North Pacific seawater is maintained by the outflow of warm-water from 8 million meters to 3 seconds per second flowing through the Indonesian waters and partly from the equator to the southern equatorial currents in the eastern part of the tropical Pacific. The North Pacific receives heat primarily in its east edge and south of 25 ° N, with major heat losses occurring in the Kuroshio area. In the presence of these heat sources and heat sinks, the average temperature distribution within the range of tropical anticyclones is maintained by the horizontal circulation of superficial shallow water at a flow rate of about 10 million meters to 3 seconds.