Role of land surface processes on Indian summer monsoon rainfall: Understanding and impact assessment

Authors

  • UC Mohanty School of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar – 752 050, India
  • HaraPrasad Nayak School of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, India-752050
  • MR Mohanty School of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, India-752050
  • Raghu Nadimpalli India Meteorological Department, Mausam Bhavan, Lodi Road, New Delhi.
  • P Sinha School of Earth Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, India-752050
  • KK Osuri Department of Earth, Ocean and Climate Science, National Institute of Technology Rourkela, India

DOI:

https://doi.org/10.54302/mausam.v74i2.6199

Keywords:

Land-atmosphere interaction, HRLDAS, Soil moisture, Soil temperature

Abstract

Indian Summer Monsoon is a synoptic-scale atmospheric circulation system manifested by the boundary forcing from both continents and tropical oceans. Unlike oceans, the land surface processes are complex in nature due to the heterogeneities in land surface characteristics and its associated feedbacks, thereby constraining theaccurate representation of the land surface in NWP models. Thus, understanding the land-atmosphere interaction becomes increasingly crucial especially during the Indian summer monsoon season due to the underlying warm and moist surface layer conducive forevapotranspiration, thereby fueling land atmosphere coupling during the season. The representation of surface heterogeneity and variability are constrained due to lack of surface measurements which necessitate development of land surface analysis. The major aimof the present studyisthree-fold;firstly, understanding land surfaces processes associated with the monsoonal rainfall events, secondly, preparation of a state-of-art high-resolution land surface data over India, andfinally, impact assessment of high-resolution land surface initialization on simulation monsoonalrainfall events. This study has implications for developing improved prediction system associated with the Indian Summer Monsoon.

Indian Summer Monsoon is a synoptic-scale atmospheric circulation system manifested by the boundary forcing from both continents and tropical oceans. Unlike oceans, the land surface processes are complex in nature due to the heterogeneities in land surface characteristics and its associated feedbacks, thereby constraining theaccurate representation of the land surface in NWP models. Thus, understanding the land-atmosphere interaction becomes increasingly crucial especially during the Indian summer monsoon season due to the underlying warm and moist surface layer conducive forevapotranspiration, thereby fueling land atmosphere coupling during the season. The representation of surface heterogeneity and variability are constrained due to lack of surface measurements which necessitate development of land surface analysis. The major aimof the present studyisthree-fold;firstly, understanding land surfaces processes associated with the monsoonal rainfall events, secondly, preparation of a state-of-art high-resolution land surface data over India, andfinally, impact assessment of high-resolution land surface initialization on simulation monsoonalrainfall events. This study has implications for developing improved prediction system associated with the Indian Summer Monsoon.

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Published

31-03-2023

How to Cite

[1]
U. Mohanty, H. . Nayak, M. . Mohanty, R. Nadimpalli, P. . Sinha, and K. Osuri, “Role of land surface processes on Indian summer monsoon rainfall: Understanding and impact assessment”, MAUSAM, vol. 74, no. 2, pp. 345–360, Mar. 2023.

Issue

Section

SPECIAL ISSUE IWM-7