【24h】

SATELLITE ALTIMETRY OF THE CASPIAN SEA

机译:卡皮海卫星测高仪

获取原文

摘要

The oscillations of the Caspian Sea level represent a result of mutually related hydrometeorological processes, which proceed not only in the sea catchment area but also far beyond it (Fig.1). The change in the tendency of the mean sea level variations that occurred in the middle 1970s, when the long-term level fall was replaced by its rapid and significant rise (Fig.2), represents an important indicator of the changes in the natural regime of the Caspian Sea [1]. Therefore, sea level monitoring and long-term forecast of the sea level changes represent an extremely important task. The aim of this presentation is to show the results of application of satellite altimetry methods to the investigation of seasonal and interannual variability of the sea level, wind speed and wave height in different parts of the Caspian Sea and Kara-Bogaz-Gol Bay, and the Volga River level. The work is based on the 1992-2004 TOPEX/Poseidon and Jason-1 data sets.
机译:里海海平面的振荡是相互关联的水文气象过程的结果,这一过程不仅在集水区进行,而且远远超出了它(图1)。 1970年代中期发生的平均海平面变化趋势的变化,当长期的海平面下降被其迅速而显着的上升所取代(图2)时,代表了自然状态变化的重要指标。里海[1]。因此,海平面监测和海平面变化的长期预测是一项极为重要的任务。本演讲的目的是展示应用卫星测高方法研究里海和卡拉-博加兹-戈尔湾不同地区海平面,风速和波高的季节和年际变化的结果,以及伏尔加河水位。这项工作基于1992-2004年TOPEX / Poseidon和Jason-1数据集。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号