Contrasting changes of snowfall in response to temperature and rainfall over two distinct geographic ranges of the Himalayas: A study using the High Asia Refined analysis data

Snow is a major source of water and its monitoring is important for hydrological applications. It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study inv...

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Veröffentlicht in:Journal of Earth System Science 2023-05, Vol.132 (2), p.79, Article 79
Hauptverfasser: Subrahmanyam, Kandula V, Srinivasulu, J, Kumar, Prashant, Bothale, Rajashree V, Sai, M V R Sesha
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container_start_page 79
container_title Journal of Earth System Science
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creator Subrahmanyam, Kandula V
Srinivasulu, J
Kumar, Prashant
Bothale, Rajashree V
Sai, M V R Sesha
description Snow is a major source of water and its monitoring is important for hydrological applications. It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study investigates the temporal variability of snowfall, temperature, and rainfall over Nubra (latitude: 34.53°–35.67°N; longitude: 76.75°–77.81°E) and Bhagirathi (latitude: 30.33°–31.45°N; longitude: 78.15°–79.47°E) basins in the Himalayan region using 30 yrs of reanalysis data (1991–2020). The High Asia Refined analysis (HAR) and Climatic Research Unit (CRU) data were used to study the snowfall and maximum air temperature variabilities, respectively, over the study basins. For rainfall, high-resolution (0.25° × 0.25°) gridded rainfall data from the India Meteorological Department is used. We have studied the annual and monthly variability of daily snowfall, temperature and rainfall over the two basins. Our analysis shows the declining trend (–2 mm/decade) of snowfall over the Nubra basin and a slightly increasing trend (0.12 mm/decade) in the Bhagirathi basin from 2004. The monthly time series in maximum temperature anomaly shows a positive trend with a maximum anomaly found to be around 2 K during the winter period. From the rainfall analysis, an increasing trend in annual rainfall is observed, especially Nubra basin showing a notable increase. Further, warming of the troposphere is found to be ~2–3 K, which is another important factor for the reduction in snowfall. Thus, positive trends in maximum temperature, rainfall and warming troposphere are the controlling factors for the declining (increasing) trend in snowfall over the Nubra (Bhagirathi) basins. Thus, the present study shows simultaneous changes in snowfall, temperature and rainfall over the Himalayan region and assumes importance in climatic applications.
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Our analysis shows the declining trend (–2 mm/decade) of snowfall over the Nubra basin and a slightly increasing trend (0.12 mm/decade) in the Bhagirathi basin from 2004. The monthly time series in maximum temperature anomaly shows a positive trend with a maximum anomaly found to be around 2 K during the winter period. From the rainfall analysis, an increasing trend in annual rainfall is observed, especially Nubra basin showing a notable increase. Further, warming of the troposphere is found to be ~2–3 K, which is another important factor for the reduction in snowfall. Thus, positive trends in maximum temperature, rainfall and warming troposphere are the controlling factors for the declining (increasing) trend in snowfall over the Nubra (Bhagirathi) basins. 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It provides meltwater to various rivers such as the Indus, Ganges, and Brahmaputra in the Himalayan region. Significant changes in snowfall variability play a pivotal role in climate. The present study investigates the temporal variability of snowfall, temperature, and rainfall over Nubra (latitude: 34.53°–35.67°N; longitude: 76.75°–77.81°E) and Bhagirathi (latitude: 30.33°–31.45°N; longitude: 78.15°–79.47°E) basins in the Himalayan region using 30 yrs of reanalysis data (1991–2020). The High Asia Refined analysis (HAR) and Climatic Research Unit (CRU) data were used to study the snowfall and maximum air temperature variabilities, respectively, over the study basins. For rainfall, high-resolution (0.25° × 0.25°) gridded rainfall data from the India Meteorological Department is used. We have studied the annual and monthly variability of daily snowfall, temperature and rainfall over the two basins. Our analysis shows the declining trend (–2 mm/decade) of snowfall over the Nubra basin and a slightly increasing trend (0.12 mm/decade) in the Bhagirathi basin from 2004. The monthly time series in maximum temperature anomaly shows a positive trend with a maximum anomaly found to be around 2 K during the winter period. From the rainfall analysis, an increasing trend in annual rainfall is observed, especially Nubra basin showing a notable increase. Further, warming of the troposphere is found to be ~2–3 K, which is another important factor for the reduction in snowfall. Thus, positive trends in maximum temperature, rainfall and warming troposphere are the controlling factors for the declining (increasing) trend in snowfall over the Nubra (Bhagirathi) basins. 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subjects Air temperature
Analysis
Annual rainfall
Annual variations
Basins
Climatic analysis
Daily precipitation
Datasets
Earth and Environmental Science
Earth Sciences
Glaciers
Hydrologic data
Hydrology
Latitude
Longitude
Maximum temperatures
Meltwater
Precipitation
Rainfall
Rainfall data
Regions
Rivers
Sea level
Snow
Snowfall
Space Exploration and Astronautics
Space Sciences (including Extraterrestrial Physics
Temperature anomalies
Temporal variability
Temporal variations
Trends
Troposphere
Variability
title Contrasting changes of snowfall in response to temperature and rainfall over two distinct geographic ranges of the Himalayas: A study using the High Asia Refined analysis data
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