Application of GNSS derived precipitable water vapour prediction in West Africa

IF 0.9 Q4 REMOTE SENSING
Akwasi Acheampong, K. Obeng
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引用次数: 5

Abstract

Abstract Atmospheric water vapour, a major component in weather systems serves as the main source for precipitation, provides latent heat which helps maintain the earth’s energy balance and a major parameter in Numerical Weather Prediction (NWP) models. An observational technique based on the Global Navigation Satellite System (GNSS) has made it possible to easily retrieve Precipitable Water (PW) at station’s antenna position with very high spatial and temporal variabilities. GNSS techniques are superior to ground-based and balloons sensors in terms of accuracy, ease of use, wider coverage and easier assimilation into NWP models. This study sought to use prediction models using daily observational data from Four (4) International GNSS Service stations in West Africa. The best prediction model can be used in cases of station outages and to predict PW over data poor regions using computed Zenith Tropospheric Delays (ZTD). gLAB software was used to process the stations’ data in Precise Point Positioning mode and PW were retrieved using station’s temperature and pressure values. Computed PW were compared against Total Column Water Vapour from ERA-Interim Reanalysis data in 2016. Correlation coefficient (R2) values ranging from 0.947 — 0.995 were obtained for the four stations. With computed PW’s, three regression models were tested to find the best-fit with PW as the dependent variable and ZTD being the independent variable. The quadratic model gave the highest R2 and lowest RMSE values as against the linear and exponential models. Time series forecasts models such as moving average, autoregressive, exponential smoothing and autoregressive integrated moving average were also employed. The forecasts results were compared against ZTD with autoregressive model reporting the highest R2 and lowest RMSE amongst the forecast models developed.
GNSS衍生水汽预报在西非的应用
摘要大气水汽是天气系统的主要组成部分,是降水的主要来源,提供的潜热有助于维持地球能量平衡,是数值天气预报(NWP)模式的主要参数。一种基于全球导航卫星系统(GNSS)的观测技术使得在空间和时间变化非常大的台站天线位置轻松地检索可降水量(PW)成为可能。GNSS技术在精度、易用性、更广泛的覆盖范围和更容易同化到NWP模型方面优于地面和气球传感器。本研究试图利用西非四(4)个国际GNSS服务站的每日观测数据使用预测模型。最好的预测模型可以用于站点中断的情况,并使用计算的天顶对流层延迟(ZTD)来预测数据贫乏地区的PW。采用gLAB软件以精确点定位方式对各站点的数据进行处理,利用各站点的温度和压力值反演PW。将计算的PW与2016年ERA-Interim Reanalysis数据中的总水柱水蒸气进行了比较。相关系数(R2)在0.947 ~ 0.995之间。通过计算PW,以PW为因变量,ZTD为自变量,对三种回归模型进行检验,找出最适合的模型。与线性和指数模型相比,二次模型给出了最高的R2和最低的RMSE值。采用了移动平均、自回归、指数平滑和自回归综合移动平均等时间序列预测模型。将预测结果与ZTD进行比较,自回归模型报告了所开发的预测模型中最高的R2和最低的RMSE。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geodetic Science
Journal of Geodetic Science REMOTE SENSING-
CiteScore
1.90
自引率
7.70%
发文量
3
审稿时长
14 weeks
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