Abstract
The Indian Summer Monsoon Rainfall (ISMR) is one of the most complex, yet stable climatic phenomena and it has enormous importance to the rhythms of life in the Indian subcontinent. The summer monsoon in Indian subcontinent exhibits a wide range of temporal variability that is often viewed as a manifestation of disturbances originated as a result of coupled ocean–land–atmosphere interactions. Although the large-scale processes through the Sea Surface Temperature (SST) variations predominantly control the atmospheric circulations leading to the summer monsoon rainfall, the regional land surface feedbacks can also influence the rainfall through surface variables such as snow, soil moisture, and evapotranspiration. Evapotranspiration over a region supplies moisture to the atmosphere, which may lead to precipitation in the same region or different regions. Therefore, any disturbance in the large-scale and regional-scale processes (that are associated with the ISMR) is reflected in terms of anomalous quantity of atmospheric moisture transport from the different evaporative sources to the Indian subcontinent. The chapter primarily discusses the role of the land surface feedback (through evapotranspiration) and the atmospheric moisture transport from different subcontinental terrestrial sources in the seasonal and sub-seasonal variability of ISMR.
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Pathak, A., Ghosh, S. (2019). Land–Atmosphere Interactions in Indian Monsoon at Sub-seasonal to Seasonal Scale. In: Singh, S., Dhanya, C. (eds) Hydrology in a Changing World. Springer Water. Springer, Cham. https://doi.org/10.1007/978-3-030-02197-9_6
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