Abstract

The causes of the pan-evaporation decline have been debated, and few researches have been carried out on the possible effect of local land use and land cover change on the regional pan-observation data series. In this paper, the urbanization effect on the estimate of pan-evaporation trends over 1961–2017 was examined for the data series of 331 urban stations, applying a previously developed dataset of the reference stations, in seven large river basins of the China mainland. The trends of pan-evaporation difference series (transformed to anomaly percentage) between urban stations and reference stations were negative and statistically significant in all of the basins, indicating that urbanization significantly reduced the pan-evaporation. The urbanization-induced trend in the whole study region was −2.54%/decade for the urban stations. Except for the Yellow River Basin and the upper Yangtze River Basin, the urbanization effects in the other five large river basins of the country are all significant, with the mid and low reaches of the Yangtze River and the Songhua River registering the largest urbanization effects of −4.08%/decade and −4.06%/decade, respectively. Since the trends of regional average series for reference stations across half of the river basins are not statistically significant, the urbanization effect is a dominant factor for the observed decline in pan-evaporation. This finding would deepen our understanding of the regional and basin-wide change in pan-evaporation observed over the last decades.

Highlights

  • Evaporation plays an important role in the Earth’s water cycle and energy cycle [1].Pan-evaporation can reflect the evaporation potential of an area, and it has great significance for estimating the actual evaporation

  • In China, change in the climatic factors including wind speed, solar radiation and diurnal temperature range has been found to keep in pace with the change of pan-evaporation, and they were considered as the direct atmospheric factors causing the reduction of pan-evaporation in the country [16,17]

  • In terms of the long-term change, each basin has a negative trend of the warm-season pan-evaporation during the past 57 years (Table 1)

Read more

Summary

Introduction

Evaporation plays an important role in the Earth’s water cycle and energy cycle [1].Pan-evaporation can reflect the evaporation potential of an area, and it has great significance for estimating the actual evaporation. The global surface air temperature has been warming rapidly in the past decades to one hundred years [2,3,4,5,6]. In this context of global warming, the evaporation should be increased. The decreased trends of pan-evaporation were observed in many regions [7,8,9,10,11,12,13], which is the well-known paradox of evaporation [14]. In China, change in the climatic factors including wind speed, solar radiation and diurnal temperature range has been found to keep in pace with the change of pan-evaporation, and they were considered as the direct atmospheric factors causing the reduction of pan-evaporation in the country [16,17]

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

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