Comparison of climatic trends and variability among glacierized environments in the Western Himalayas
      
      
        
      
      
      
      
        
          
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Dimri, A. P.
School of Environmental Sciences, Jawaharlal Nehru University, New Delhi, India
          
 
          
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Immerzeel, W. W.
Department of Geosciences, Utrecht University, Netherlands
          
 
          
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Salzmann, Nadine
  Department of Geography, University of Fribourg, Switzerland
          
 
          
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Thayyen, R. J.
National Institute of Hydrology, Roorkee, India
          
 
          
        
        
       
      
      
      
      
      
      
      
      
      
      
      
      
      
      
      
        
        Published in:
        
          
            
            - Theoretical and Applied Climatology. - 2018, vol. 134, no. 1, p. 155–163
 
            
          
         
       
      
      
      
       
      
      
      
        
        English
        
        
        
          The climate and hydrology of the Western Himalayas is complex and a function of  snow and glacier melt, land use, topography, and Indian summer and winter monsoon  dynamics. Improving our knowledge about these processes is important from societal  and agricultural points of view. In this study, an observational analysis is carried out to  assess the changing climatic trends and the associated interannual variability in winter  temperature and precipitation at three glacierized regions of Western Himalayas  having distinctly different sub-regional characteristics. In situ observations of 23 years  (1985–2007) are used. These observations are passed through rigorous statistical  quality control checks. Results show higher interannual variability with increasing  temperature trends in the glacierized regions of the Siachen (Karakoram Range) and  Chotasigri (Great Himalayan Range). Karakoram Range has higher warming trends  than the Great Himalayan Range. In case of precipitation, an overall decrease in  precipitation is observed with contrasting trends in the last decade. Nino3.4 index is  positively correlated with winter precipitation with similar interannual variability. In  addition, at Siachen temperature and precipitation show strong negative correlation,  and precipitation to spell length correlation is opposite at Siachen and Chotasigri.
        
        
       
      
      
      
        
        
        
        
        
        
        
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          Faculty
          
        
 
        - Faculté des sciences et de médecine
 
        
        
        
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          Department
          
        
 
        - Département de Géosciences
 
        
        
        
        
        
        
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                  Meteorology, climatology
                
              
            
          
        
 
        
        
        
          
        
        
        
          
        
        
        
        
        
        
        
        
        
        
        
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          Persistent URL
        
 
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          https://folia.unifr.ch/unifr/documents/307454
        
 
      
     
   
  
  
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