Spatiotemporal Precipitation Trends and Associated Large-Scale Teleconnections in Northern Pakistan

Document Type : Abstract

Authors

1 Jianshui Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China; Key Laboratory of State Forestry and Grassland Administration on Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China

2 International Research Center on Karst under the auspices of UNESCO; Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China

3 Department of Applied Mathematics, Chung Yuan Christian University Chung-Li 541004, Taiwan

4 Defense and Security, Rabdan Academy, Abu Dhabi 114646, United Arab Emirates

5 Synthesis Research Centre of Chinese Ecosystem Research Network, Key Laboratory of Ecosystem Network Observation and Modelling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China

6 Department of Atmospheric and Oceanic Sciences and & Institute of Atmospheric Sciences, Fudan University, Shanghai 200433, China

Abstract

Background and Aim: Climate change poses unprecedented challenges, impacting food production and increasing flood risks. This study focuses on northern Pakistan, assessing observed changes in seasonal and annual precipitation using data from 25 meteorological stations and ERA-5 reanalysis. The aim is to understand spatial trends, analyze oceanic indices' association with precipitation, and provide insights for water resource management.
Method: Monthly precipitation data and ERA-5 reanalysis complemented unevenly distributed station data. Trend assessments utilized non-parametric tests (MK, SSE, SQMK), and wavelet analysis explored oceanic index associations from 1960 to 2016.
Results: Max precipitation occurred in annual and summer seasons. Overall, NP experienced declining annual, winter, spring, and summer precipitation but an autumn increase at 0.43 mm/decade (1989–2016). Spatial trends aligned in winter, spring, and autumn but diverged in summer and annual trends. Region III saw significant summer and annual increases (1989–2016), contrasting overall NP decreases (1960–2016). An increase in annual precipitation post-1985 was observed, with elevation-dependent variations.
Conclusion: Interannual coherence of precipitation with ENSO, AO, and PDO was noted. Winter and spring precipitation correlated with AO and ENSO, while summer precipitation linked to IOD and PDO. The findings inform water resource management policies in NP amid climate change, emphasizing the need for adaptive strategies to ensure sustainable water resources.

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Volume 2, Issue 2
Special Issue: Abstract and Papers from ICLS23 (Turkey), ICNFEAS23 (Turkey)
Pages 329-329
  • Receive Date: 20 December 2023
  • Accept Date: 20 December 2023