Variability, Trends and Return Periods of Extreme Rainfall Events (EREs) over the North-Western Indian Himalayan Region (NW-IHR)
Author:
Funder
Ministry of Education, Government of India
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00024-024-03542-9.pdf
Reference72 articles.
1. Adarsh, S., & Janga Reddy, M. (2015). Trend analysis of rainfall in four meteorological subdivisions of southern India using nonparametric methods and discrete wavelet transforms. International Journal of Climatology, 35(6), 1107–1124. https://doi.org/10.1002/joc.4042
2. Bao, J., Sherwood, S. C., Alexander, L. V., & Evans, J. P. (2017). Future increases in extreme precipitation exceed observed scaling rates. Nature Climate Change, 7(2), 128–132. https://doi.org/10.1038/nclimate3201
3. Basistha, A., Arya, D. S., & Goel, N. K. (2008). Spatial distribution of rainfall in Indian Himalayas–a case study of UK region. Water Resources Management, 22(10), 1325–1346. https://doi.org/10.1007/s11269-007-9228-2
4. Bharti, V., Singh, C., Ettema, J., & Turkington, T. A. R. (2016). Spatiotemporal characteristics of EREs over the Northwest Himalaya using satellite data. International Journal of Climatology, 36(12), 3949–3962. https://doi.org/10.1002/joc.4605
5. Bookhagen, B., & Burbank, D. W. (2010). Toward a complete Himalayan hydrological budget: Spatiotemporal distribution of snowmelt and rainfall and their impact on river discharge. Journal of Geophysical Research Earth Surface. https://doi.org/10.1029/2009JF001426
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