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Diurnal and seasonal variation of heat fluxes over an agricultural field in southeastern Nepal

  • Ram Hari Acharya
  • Madan SigdelEmail author
  • Yaoming MaEmail author
  • Binbin Wang
Article
  • 52 Downloads

Abstract

The southeastern part of Nepal is traditionally known as the entrance of the South Asian summer monsoon system (SASM) and plays a vital role in the development of the national agro-economy. This research examined the diurnal and seasonal variation in the heat and mass fluxes. The study area lies in the agricultural fields that maintain crop cycles. Half-hourly data for a period of 54 months starting in October 2012 were obtained from the Tarahara surface flux observation system (SFOS), and the analyzed data included fast response eddy covariance measurements. The results show that all radiation components changed diurnally and seasonally, except for downward longwave radiation, which revealed weak diurnal variation during winter months. The winter surface albedo of the agricultural field was higher than the summer surface albedo and varied from 0.13 to 0.19. Latent heat release was found to be strongest during the summer season and was associated with atmospheric moisture content and precipitation. Sensible heat becomes weaker during summer and exhibits significant variation during winter months. The sensible heat flux increased rapidly with the increasing radiation flux during the pre-monsoon, which is a major energy source for driving atmospheric systems. The partitioning of energy into turbulent fluxes was also analyzed and it was found that the released latent heat consumed 67% of the net radiation; furthermore, 21% was consumed by the released sensible heat. The response of the land surface heat fluxes to the large-scale circulation system was clearly identified on the basis of the highest peak values observed in 2015 and 2016.

Notes

Acknowledgments

The authors acknowledge the Central Department of Hydrology and Meteorology, Tribhuvan University for providing a research platform and the Institute of Tibetan Plateau Research, Chinese Academy of Sciences for managing the surface flux data. We would like to thank Dr. Pukar Man Amatya for establishment and regular maintenance of surface flux observation system in Tarahara.

Funding information

This research was funded by the National Natural Science Foundation of China (41661144043) and the Chinese Academy of Sciences (Grant No. QYZDJ-SSW-DQC019). First author was financially supported by KCRE excellent student thesis grants award 2017 during his M.Sc.

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Copyright information

© Springer-Verlag GmbH Austria, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Central Department of Hydrology and MeteorologyTribhuvan UniversityKathmanduNepal
  2. 2.Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijingChina
  3. 3.CAS Center for Excellence in Tibetan Plateau Earth ScienceBeijingChina
  4. 4.University of Chinese Academy of SciencesBeijingChina

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