Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time Series

Precipitable water vapor (PWV) is a meteorological variable that influences the main processes that occur in the atmosphere. It is not a homogeneous variable, but varies both temporally and spatially according to local conditions. This study analyzes the spatial and temporal variability of the PWV i...

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Main Authors: Katherine L. Ccoica-López, Jose J. Pasapera-Gonzales, Juan C. Jimenez
Format: Article
Language:English
Published: MDPI AG 2019-04-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/10/4/192
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spelling doaj-b300f405bcc74fc288a37f0020e4c80b2020-11-25T00:30:03ZengMDPI AGAtmosphere2073-44332019-04-0110419210.3390/atmos10040192atmos10040192Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time SeriesKatherine L. Ccoica-López0Jose J. Pasapera-Gonzales1Juan C. Jimenez2Department of Physics, Environmental Engineering and Meteorology, National Agrarian University La Molina, Lima 15024, PeruSpace Agency of Perú, National Commission for Aerospace Research and Development, CONIDA, Lima 15046, PeruImage Processing Laboratory, Global Change Unit, University of Valencia, Valencia 46980, SpainPrecipitable water vapor (PWV) is a meteorological variable that influences the main processes that occur in the atmosphere. It is not a homogeneous variable, but varies both temporally and spatially according to local conditions. This study analyzes the spatial and temporal variability of the PWV in Peru using MODIS satellite data (MOD05/MYD05 products) during the period 2000 to 2017. MODIS-derived PWV values were complemented with ERA-Interim reanalysis data to take the study period back to 1979. PWV values extracted from MODIS and ERA-Interim were compared against in situ values obtained from five radiosonde stations between the years of 2003 and 2016 (non-continuous data). The study was performed over nine sub-regions of the Peruvian territory: coastal, highland, and jungle sub-regions, which in turn were classified into northern, central and southern regions. The analysis of spatial variability was performed using monthly semivariograms and influencing parameters such as sill and range, whereas the temporal variation was examined by time series of monthly, seasonal, and multi-annual means. The Mann-Kendall test was also applied to determine the presence of trends. The spatial analysis evidenced the heterogeneity of the PWV over the study region, and in most of the sub-regions there was directional variability during the austral summer and austral winter, with the Northeast (NE) and East (E) directions having the greatest spatial variability. The omnidirectional analysis of the sill and range showed that there was a high spatial variability of PWV mainly over the northern and southern jungle, even exceeding the limit area of these sub-regions. The temporal analysis shows that this variability occurs more in the north and center of the jungle and in the north coast, where the content of PWV is higher in relation to other regions, while the central and southern highlands have the lowest values. In addition, the trend test determines that there is a slight increase in PWV for the coast and jungle regions of Peru. Validation analysis using the radiosonde data showed a similar performance of both datasets (MODIS and ERA), with better results for the case of the MODIS product (RMSE &lt; 0.6 cm and R<sup>2</sup> = 0.71).https://www.mdpi.com/2073-4433/10/4/192precipitable water vaporMODISERA interimtrend analysis
collection DOAJ
language English
format Article
sources DOAJ
author Katherine L. Ccoica-López
Jose J. Pasapera-Gonzales
Juan C. Jimenez
spellingShingle Katherine L. Ccoica-López
Jose J. Pasapera-Gonzales
Juan C. Jimenez
Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time Series
Atmosphere
precipitable water vapor
MODIS
ERA interim
trend analysis
author_facet Katherine L. Ccoica-López
Jose J. Pasapera-Gonzales
Juan C. Jimenez
author_sort Katherine L. Ccoica-López
title Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time Series
title_short Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time Series
title_full Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time Series
title_fullStr Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time Series
title_full_unstemmed Spatio-Temporal Variability of the Precipitable Water Vapor over Peru through MODIS and ERA-Interim Time Series
title_sort spatio-temporal variability of the precipitable water vapor over peru through modis and era-interim time series
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2019-04-01
description Precipitable water vapor (PWV) is a meteorological variable that influences the main processes that occur in the atmosphere. It is not a homogeneous variable, but varies both temporally and spatially according to local conditions. This study analyzes the spatial and temporal variability of the PWV in Peru using MODIS satellite data (MOD05/MYD05 products) during the period 2000 to 2017. MODIS-derived PWV values were complemented with ERA-Interim reanalysis data to take the study period back to 1979. PWV values extracted from MODIS and ERA-Interim were compared against in situ values obtained from five radiosonde stations between the years of 2003 and 2016 (non-continuous data). The study was performed over nine sub-regions of the Peruvian territory: coastal, highland, and jungle sub-regions, which in turn were classified into northern, central and southern regions. The analysis of spatial variability was performed using monthly semivariograms and influencing parameters such as sill and range, whereas the temporal variation was examined by time series of monthly, seasonal, and multi-annual means. The Mann-Kendall test was also applied to determine the presence of trends. The spatial analysis evidenced the heterogeneity of the PWV over the study region, and in most of the sub-regions there was directional variability during the austral summer and austral winter, with the Northeast (NE) and East (E) directions having the greatest spatial variability. The omnidirectional analysis of the sill and range showed that there was a high spatial variability of PWV mainly over the northern and southern jungle, even exceeding the limit area of these sub-regions. The temporal analysis shows that this variability occurs more in the north and center of the jungle and in the north coast, where the content of PWV is higher in relation to other regions, while the central and southern highlands have the lowest values. In addition, the trend test determines that there is a slight increase in PWV for the coast and jungle regions of Peru. Validation analysis using the radiosonde data showed a similar performance of both datasets (MODIS and ERA), with better results for the case of the MODIS product (RMSE &lt; 0.6 cm and R<sup>2</sup> = 0.71).
topic precipitable water vapor
MODIS
ERA interim
trend analysis
url https://www.mdpi.com/2073-4433/10/4/192
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AT josejpasaperagonzales spatiotemporalvariabilityoftheprecipitablewatervaporoverperuthroughmodisanderainterimtimeseries
AT juancjimenez spatiotemporalvariabilityoftheprecipitablewatervaporoverperuthroughmodisanderainterimtimeseries
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