Please use this identifier to cite or link to this item: https://dspace.iiti.ac.in/handle/123456789/6317
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dc.contributor.authorGoyal, Manish Kumaren_US
dc.date.accessioned2022-03-17T01:00:00Z-
dc.date.accessioned2022-03-21T10:46:15Z-
dc.date.available2022-03-17T01:00:00Z-
dc.date.available2022-03-21T10:46:15Z-
dc.date.issued2020-
dc.identifier.citationSharma, A., & Goyal, M. K. (2020). Assessment of the changes in precipitation and temperature in teesta river basin in indian himalayan region under climate change. Atmospheric Research, 231 doi:10.1016/j.atmosres.2019.104670en_US
dc.identifier.issn0169-8095-
dc.identifier.otherEID(2-s2.0-85072198467)-
dc.identifier.urihttps://doi.org/10.1016/j.atmosres.2019.104670-
dc.identifier.urihttps://dspace.iiti.ac.in/handle/123456789/6317-
dc.description.abstractThe Himalayas, also known as the third pole on Earth, are vulnerable to climatic changes due to the presence of a large number of glaciers and glacial lakes. Here, we examined the changes in precipitation, temperature and climate extremes (23 indices) in the Teesta River basin in Eastern Himalayas for the period 1951–2100. We used four different General Circulation Models (GCMs) with two Representative Concentration Pathways (RCP4.5 and RCP8.5). We found substantial changes in precipitation, temperature and climate extreme patterns for both observed and projected climates. In general, warming and increase in precipitation were found, which increases from RCP4.5 to RCP8.5. The basin-average maximum and minimum daily temperatures are expected to increase by 0.54 °C, 1.18 °C and 1.92 °C, and 0.5 °C, 1.2 °C and 2 °C for period 2011–2040, 2041–2070, and 2071–2100, respectively, compared to 1951–2010 period under RCP8.5. Precipitation is likely to increase in both monsoon and non-monsoon seasons; however, there is large uncertainty associated with projections. Significant increase in precipitation indices, such as RX1day, RX5day, R10, R20, CWD and R95p, is projected under RCPs over the 21st century. Decrease in cool events, such as cool nights, cool days, frost days and ice days, and increase in warm events, such as warm nights, warm days, summer days and tropical nights, are projected under RCPs. In addition, the snowfall contribution to precipitation is likely to decrease drastically, which might result in water availability issues. Our results are in agreement with previous studies in and around the basin. © 2019en_US
dc.language.isoenen_US
dc.publisherElsevier Ltden_US
dc.sourceAtmospheric Researchen_US
dc.subjectAtmospheric thermodynamicsen_US
dc.subjectWatershedsen_US
dc.subjectClimate extremesen_US
dc.subjectDaily temperaturesen_US
dc.subjectGeneral circulation modelen_US
dc.subjectHimalayasen_US
dc.subjectIndian Himalayan Regionen_US
dc.subjectPrecipitation indicesen_US
dc.subjectSikkimen_US
dc.subjectWater availabilityen_US
dc.subjectClimate changeen_US
dc.subjectclimate changeen_US
dc.subjectclimate modelingen_US
dc.subjectextreme eventen_US
dc.subjectgeneral circulation modelen_US
dc.subjectmonsoonen_US
dc.subjectprecipitation (climatology)en_US
dc.subjecttemperature profileen_US
dc.subjectHimalayasen_US
dc.subjectSikkim Himalayasen_US
dc.subjectTeesta Riveren_US
dc.titleAssessment of the changes in precipitation and temperature in Teesta River basin in Indian Himalayan Region under climate changeen_US
dc.typeJournal Articleen_US
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