Abstract

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 < 0.6 cm and R2 = 0.71).

Highlights

  • Water vapour is an atmospheric constituent, and the factor responsible for humidity in the environment and the greenhouse effect [1,2,3,4,5]

  • Precipitable Water Vapour (PWV) refers to the integration of water vapour along the atmospheric column, and is indicative of the water vapour amount that may be potentially converted to precipitation

  • This study provided one of the first detailed analyses of spatio-temporal variations of PWV over

Read more

Summary

Introduction

Water vapour is an atmospheric constituent, and the factor responsible for humidity in the environment and the greenhouse effect [1,2,3,4,5]. Precipitable Water Vapour (PWV) refers to the integration of water vapour along the atmospheric column, and is indicative of the water vapour amount that may be potentially converted to precipitation. Atmosphere 2019, 10, 192 pattern, especially over oceans, where the PWV amount is higher over the Equator and lower over the Poles. Over continental lands there is a significant influence of the orography, with the Atmosphere 2019, 10 FOR PEER REVIEW lowest values over high altitude sites and locations far away from the sea, and the highest values over low elevation and sites near over the coast.

Objectives
Methods
Results
Conclusion

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.