Trends in temperature, diurnal temperature range and sunshine duration in Northeast India

被引:141
作者
Jhajharia, Deepak [1 ]
Singh, Vijay P. [2 ,3 ]
机构
[1] N Eastern Reg Inst Sci & Technol, Dept Agr Engn, Itanagar 791109, Arunachal Prade, India
[2] Texas A&M Univ, Dept Biol & Agr Engn, College Stn, TX 77843 USA
[3] Texas A&M Univ, Dept Civil & Environm Engn, College Stn, TX 77843 USA
关键词
trend; temperature; diurnal temperature range; sunshine duration; Northeast India; SURFACE AIR-TEMPERATURE; LONG-TERM TRENDS; CLIMATE-CHANGE; PAN EVAPORATION; MAXIMUM; MINIMUM; EVAPOTRANSPIRATION; ASYMMETRY; HIMALAYA; MALARIA;
D O I
10.1002/joc.2164
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Trends in maximum (T-max), minimum (T-min) and mean (T-mean) temperatures; diurnal temperature range (DTR = T-max - T-min); and sunshine duration at eight sites in Northeast (NE) India were investigated. Three sites observed decreasing trends in DTR corresponding to annual, seasonal (pre-monsoon and monsoon) and monthly (September) time scales. On the other hand, DTR increases were also observed at other three sites in monsoon and post-monsoon seasons as well as in the months of June, October and December. The sites showing DTR decreases (increases) witnessed either increasing trends in T-min (T-max) or decreasing trends in T-max (T-min), with T-max (T-min) showing either no trend or increasing at a smaller rate than T-min (T-max). Temperature remained practically trendless in winter and pre-monsoon seasons over NE India. However, temperature increases were observed in monsoon and post-monsoon seasons. Decreasing trends in sunshine duration were observed mainly on annual, seasonal (winter and pre-monsoon) and monthly (January, February and March) time scales. Concomitant decreases in sunshine duration may be one of the potential causes of the observed DTR decreases over NE India. Copyright (C) 2010 Royal Meteorological Society
引用
收藏
页码:1353 / 1367
页数:15
相关论文
共 63 条
[1]   Man-made climatic changes in the Ganges basin [J].
Adel, MM .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2002, 22 (08) :993-1016
[2]  
Ahmad QK., 1996, IMPLICATIONS CLIMATE
[3]  
ANGELL JK, 1990, J CLIMATE, V3, P296, DOI 10.1175/1520-0442(1990)003<0296:VIUSCA>2.0.CO
[4]  
2
[5]   Temporal and spatial trends of temperature patterns in Israel [J].
Ben-Gai, T ;
Bitan, A ;
Manes, A ;
Alpert, P ;
Rubin, S .
THEORETICAL AND APPLIED CLIMATOLOGY, 1999, 64 (3-4) :163-177
[6]  
Bhutiyani MR, 2007, CLIMATIC CHANGE, V85, P159, DOI [10.1007/s10584-006-9196-1, 10.1007/S10584-006-9196-1]
[7]   Climatic variables and transmission of malaria: A 12-year data analysis in Shuchen County, China [J].
Bi, P ;
Tong, SL ;
Donald, K ;
Parton, KA ;
Ni, JF .
PUBLIC HEALTH REPORTS, 2003, 118 (01) :65-71
[8]   Diurnal temperature range as an index of global climate change during the twentieth century [J].
Braganza, K ;
Karoly, DJ ;
Arblaster, JM .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (13) :L132171-4
[9]   Evaporation and potential evapotranspiration in India under conditions of recent and future climate change [J].
Chattopadhyay, N ;
Hulme, M .
AGRICULTURAL AND FOREST METEOROLOGY, 1997, 87 (01) :55-73
[10]  
Cohen S, 1996, J APPL METEOROL, V35, P1051, DOI 10.1175/1520-0450(1996)035<1051:CCCITJ>2.0.CO