21st Century climate change projections of temperature and precipitation in Central Kashmir Valley under RCP 4.5 and RCP 8.5

IF 0.7 4区 地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
MAUSAM Pub Date : 2023-10-01 DOI:10.54302/mausam.v74i4.4264
SYED ROUHULLAH ALI, JUNAID N. KHAN, ROHITASHW KUMAR, FAROOQ AHMAD LONE, SHAKEEL AHMAD MIR, IMRAN KHAN
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引用次数: 0

Abstract

Regional climate models (RCMs) give more reliable results for a regional impact study of climate change, but they still have a significant bias that has to be corrected before they can be utilised in climate change research. In this study, two methods for local bias correction of Tmax, Tmin and precipitation data at monthly scales, namely the modified difference approach (MDA) and the linear scaling (LS) method, were applied and validated to minimize the bias between the modelled (HAD GEM2-ES-GCM) and observed climate data in Central Kashmir Valley. Tmax, Tmin and precipitation correction functions generated using the LS method on a monthly time scale were shown to be excellent than MDA for bias correction of weather data to make it close to observed data in both scenarios (RCP 4.5 & 8.5). Comparison between two scenarios was done to determine the climate change extent in Central Kashmir Valley using LS method. The past 30 years observed average temperature and precipitation was 14.17 °C and 734.06 mm, respectively considered as a baseline for comparison purpose. Annual Taverage (°C) showed increase in all the three time slices and maximum increase by 3.09 and 5.72 °C during far future (FF) (2071-2095) under RCP 4.5 & 8.5, respectively. Whereas, the results of average annual precipitation also showed increase in future scenario and maximum increase by 29.25 mm (3.98%) during mid future (2046-2070) and 215.98 mm (29.42%) during end future (2071-2095), under RCP 4.5 & 8.5 respectively. It was concluded that under RCP 8.5 scenario climate change was quite significant than RCP 4.5.
RCP 4.5和RCP 8.5下克什米尔中部山谷21世纪气温和降水的气候变化预估
区域气候模式(RCMs)为气候变化的区域影响研究提供了更可靠的结果,但是它们仍然存在显著的偏差,必须在将其用于气候变化研究之前加以纠正。本文采用修正差分法(MDA)和线性标度法(LS)对月尺度上的Tmax、Tmin和降水数据进行局地偏差校正,以最大限度地减小模拟(HAD GEM2-ES-GCM)与观测数据之间的偏差。使用LS方法生成的月时间尺度上的Tmax、Tmin和降水校正函数比MDA对天气数据的偏差校正更优,使其接近两种情景下的观测数据(RCP 4.5 &8.5)。利用LS方法对两种情景进行比较,确定了克什米尔中部谷地的气候变化程度。过去30年的平均气温和降水分别为14.17°C和734.06 mm,作为比较的基线。在RCP 4.5 &下,年平均(°C)在远未来(FF)(2071-2095)期间均呈上升趋势,最大增幅分别为3.09和5.72°C;8.5,分别。而在RCP 4.5 &条件下,未来情景的年平均降水量也呈现增加趋势,未来中期(2046 ~ 2070年)和未来末期(2071 ~ 2095年)最大增幅分别为29.25 mm(3.98%)和215.98 mm (29.42%);分别为8.5。结果表明,RCP 8.5情景下的气候变化显著高于RCP 4.5情景。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
MAUSAM
MAUSAM 地学-气象与大气科学
CiteScore
1.20
自引率
0.00%
发文量
1298
审稿时长
6-12 weeks
期刊介绍: MAUSAM (Formerly Indian Journal of Meteorology, Hydrology & Geophysics), established in January 1950, is the quarterly research journal brought out by the India Meteorological Department (IMD). MAUSAM is a medium for publication of original scientific research work. MAUSAM is a premier scientific research journal published in this part of the world in the fields of Meteorology, Hydrology & Geophysics. The four issues appear in January, April, July & October.
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