GIS-based high-resolution spatial interpolation of precipitation in mountain–plain areas of Upper Pakistan for regional climate change impact studies

被引:10
作者
Muhammad Waseem Ashiq
Chuanyan Zhao
Jian Ni
Muhammad Akhtar
机构
[1] Punjab Forest Department,Institute of Geology
[2] University of the Punjab (PU),Key Laboratory of Arid and Grassland Agroecology of Ministry of Education
[3] Lanzhou University,Centre for Forest Conservation Genetics, Department of Forest Sciences
[4] Max Planck Institute for Biogeochemistry,undefined
[5] Alfred Wegener Institute for Polar and Marine Research,undefined
[6] University of British Columbia (UBC),undefined
来源
Theoretical and Applied Climatology | 2010年 / 99卷
关键词
Root Mean Square Error; Regional Climate Model; Baseline Period; Ordinary Kriging; Cokriging;
D O I
暂无
中图分类号
学科分类号
摘要
In this study, the baseline period (1960–1990) precipitation simulation of regional climate model PRECIS is evaluated and downscaled on a monthly basis for northwestern Himalayan mountains and upper Indus plains of Pakistan. Different interpolation models in GIS environment are used to generate fine scale (250 × 250 m2) precipitation surfaces from PRECIS precipitation data. Results show that the multivariate extension model of ordinary kriging that uses elevation as secondary data is the best model especially for monsoon months. Model results are further compared with observations from 25 meteorological stations in the study area. Modeled data show overall good correlation with observations confirming the ability of PRECIS to capture major precipitation features in the region. Results for low and erratic precipitation months, September and October, are however showing poor correlation with observations. During monsoon months (June, July, August) precipitation pattern is different from the rest of the months. It increases from south to north, but during monsoon maximum precipitation is in the southern regions of the Himalayas, and extreme northern areas receive very less precipitation. Modeled precipitation toward the end of the twenty-first century under A2 and B2 scenarios show overall decrease during winter and increase in spring and monsoon in the study area. Spatially, both scenarios show similar pattern but with varying magnitude. In monsoon, the Himalayan southern regions will have more precipitation, whereas northern areas and southern plains will face decrease in precipitation. Western and south western areas will suffer from less precipitation throughout the year except peak monsoon months. T test results also show that changes in monthly precipitation over the study area are significant except for July, August, and December. Result of this study provide reliable basis for further climate change impact studies on various resources.
引用
收藏
页码:239 / 253
页数:14
相关论文
共 151 条
  • [1] Agnew MD(2000)GIS based construction of baseline climatologies for the Mediterranean using terrain variables Clim Res 14 115-127
  • [2] Palutikof JP(2008)Use of regional climate model simulations as input for hydrological models for the Hindukush–Karakorum–Himalaya region Hydrology and Earth System Sciences Discussions 5 865-902
  • [3] Akhtar M(2001)Hilbertian approach for univariate spline with tension Approx Theory its Appl 17 36-57
  • [4] Ahmad N(2003)Simulation of high latitude hydrological processes in the Torne–Kalix basin: PILPS Phase 2(e): 1. Experiment description and summary intercomparisons Glob Planet Change 38 1-30
  • [5] Booij MJ(2001)Spatial variations in the average rainfall–altitude relationship in Great Britain: an approach using geographically weighted regression Int J Climatol 21 455-466
  • [6] Bouhamidi A(2001)Performance of statistical downscaling models in GCM validation and regional climate change estimates: application for Swedish precipitation Int J Climatol 21 557-578
  • [7] Bowling LC(1999)Validation of downscaling models for changed climate conditions: case study of southwestern Australia Clim Res 12 1-14
  • [8] Lettenmaier DP(1998)Sensitivity of ecosystem models to the spatial resolution of the NCAR Community Climate Model CCM2 Clim Dyn 14 409-429
  • [9] Nijssen B(1998)High-resolution studies of rainfall on Norfolk Island Part II: interpolation of rainfall data J Hydrol 208 187-193
  • [10] Graham LP(2000)An improved statistical-dynamical downscaling scheme and its application to the alpine precipitation climatology Theor Appl Climatol 65 119-135