一种利用子卫星测量进行船舶导航区卫星水文气象信息业务校正的方法

D. Akmaykin, V. Grinyak, Viktoriya Valer'evna Bocharova, Oleg Alekseevich Bukin
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引用次数: 0

摘要

本文考虑了通过卫星和船舶测量相结合来评估海面状况的问题。有关海面风力和风向的信息对于确保航行安全和规划船只过境路线非常重要。它对天气预报和刺激也至关重要。风力数据传统上是从过往船只和浮标上获取的。船只数据只覆盖世界海洋的有限区域,而且接收不均,浮标数据非常稀少,因此无法充分了解大气洋流的分布情况。遥感卫星的使用使风速和风向的测量密度增加了几个数量级,也使所获得数据的相关性得到提高。然而,卫星测量可能会失真。特别是大气降水(雨)的影响会使风速测量误差增加两倍。强风和弱风也会造成问题:在强风中,测量数据会低估真实风速,而在弱风中则会高估风速。本文提出了一种修正风速和风向卫星数据的方法。该方法的实质是将子卫星船的测量数据与卫星信息结合起来使用。通过了解当地(从船上)测量的天气数据,可以计算出修正卫星数据的回归参数。将计算出的参数应用于水域卫星图像的回归,可以获得更准确的船舶航线区域的天气数据。本文介绍了根据鄂霍次克海水域的真实卫星数据和船上数据进行计算的结果。采用二次多项式作为回归函数。结果表明,与直接从卫星接收到的数据相比,利用子卫星船舶测量数据进行的修正能更准确地描述波浪的特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A method of satellite hydrometeorological information operational correction in a ship's navigation area using sub-satellite measurements
The problem of assessing the state of the sea surface by combining satellite and ship measurements is considered. Information about the strength and direction of the wind at the sea surface is important to ensure safe navigation and planning of vessel transit routes. It is of key importance for weather forecasting and excitement. Wind data is traditionally obtained from passing ships and buoys. Ship data covers only limited areas of the World Ocean and is received unevenly, buoy data is highly sparse, which makes it impossible to obtain an adequate picture of the distribution of atmospheric currents. The use of remote sensing satellites has made it possible to increase the density of measurements of wind speed and direction by orders of magnitude, and the relevance of the data obtained. However, satellite measurements can be distorted. In particular, the influence of atmospheric precipitation (rain) can give a two-fold error in measuring wind speed. Strong and weak winds also create problems: in strong winds, the measured data underestimate the true wind speed, in weak winds they overestimate. A method for correcting satellite data on wind speed and direction is proposed. The essence of the method is to use subsatellite ship measurements in conjunction with satellite information. Knowing the weather data measured locally (from the ship), it is possible to calculate regression parameters for correcting satellite data. By applying regressions with calculated parameters to satellite images in the water area, it is possible to obtain more accurate weather data in the area of the vessel's route. The results of calculations based on real satellite and on-board data in the waters of the Sea of Okhotsk are presented. A polynomial of the second degree is taken as a regression function. It is shown that the correction using subsatellite ship measurements more accurately characterizes the wave than the data directly received from the satellite.
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