Evidence of trends in daily climate extremes over southern and west Africa

被引:461
作者
New, Mark
Hewitson, Bruce
Stephenson, David B.
Tsiga, Alois
Kruger, Andries
Manhique, Atanasio
Gomez, Bernard
Coelho, Caio A. S.
Masisi, Dorcas Ntiki
Kululanga, Elina
Mbambalala, Ernest
Adesina, Francis
Saleh, Hemed
Kanyanga, Joseph
Adosi, Juliana
Bulane, Lebohang
Fortunata, Lubega
Mdoka, Marshall L.
Lajoie, Robert
机构
[1] Univ Oxford, Ctr Environm, Oxford OX1 3QY, England
[2] Univ Cape Town, Dept Geog & Environm Sci, ZA-7925 Cape Town, South Africa
[3] Univ Reading, Dept Meteorol, Reading RG6 6BB, Berks, England
[4] Natl Meteorol Serv, Harare, Zimbabwe
[5] S Africa Weather Serv, ZA-0001 Pretoria, South Africa
[6] Natl Meteorol Serv, Maputo, Mozambique
[7] Dept Water Resources, Banjul, Gambia
[8] Natl Meteorol Serv, Bechuanaland, Botswana
[9] Natl Meteorol Serv, Chileka, Malawi
[10] Obafemi Awolowo Univ, Dept Geog, Ife, Nigeria
[11] Tanzanian Meteorol Agcy, Dar Es Salaam, Tanzania
[12] Zambia Meteorol Dept, Lusaka 10101, Zambia
[13] Lesotho Meteorol Serv, Maseru 100, Lesotho
[14] Uganda Meteorol Dept, Kampala, Uganda
[15] Natl Meteorol Serv, Victoria, Seychelles
关键词
D O I
10.1029/2005JD006289
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[ 1] There has been a paucity of information on trends in daily climate and climate extremes, especially from developing countries. We report the results of the analysis of daily temperature ( maximum and minimum) and precipitation data from 14 south and west African countries over the period 1961 - 2000. Data were subject to quality control and processing into indices of climate extremes for release to the global community. Temperature extremes show patterns consistent with warming over most of the regions analyzed, with a large proportion of stations showing statistically significant trends for all temperature indices. Over 1961 to 2000, the regionally averaged occurrence of extreme cold ( fifth percentile) days and nights has decreased by - 3.7 and - 6.0 days/decade, respectively. Over the same period, the occurrence of extreme hot (95th percentile) days and nights has increased by 8.2 and 8.6 days/decade, respectively. The average duration of warm ( cold) has increased ( decreased) by 2.4 (0.5) days/decade and warm spells. Overall, it appears that the hot tails of the distributions of daily maximum temperature have changed more than the cold tails; for minimum temperatures, hot tails show greater changes in the NW of the region, while cold tails have changed more in the SE and east. The diurnal temperature range (DTR) does not exhibit a consistent trend across the region, with many neighboring stations showing opposite trends. However, the DTR shows consistent increases in a zone across Namibia, Botswana, Zambia, and Mozambique, coinciding with more rapid increases in maximum temperature than minimum temperature extremes. Most precipitation indices do not exhibit consistent or statistically significant trends across the region. Regionally averaged total precipitation has decreased but is not statistically significant. At the same time, there has been a statistically significant increase in regionally averaged daily rainfall intensity and dry spell duration. While the majority of stations also show increasing trends for these two indices, only a few of these are statistically significant. There are increasing trends in regionally averaged rainfall on extreme precipitation days and in maximum annual 5-day and 1-day rainfall, but only trends for the latter are statistically significant.
引用
收藏
页数:11
相关论文
共 42 条
[1]   Changes in precipitation and temperature extremes in Central America and northern South America, 1961-2003 -: art. no. D23107 [J].
Aguilar, E ;
Peterson, TC ;
Obando, PR ;
Frutos, R ;
Retana, JA ;
Solera, M ;
Soley, J ;
García, IG ;
Araujo, RM ;
Santos, AR ;
Valle, VE ;
Brunet, M ;
Aguilar, L ;
Alvarez, L ;
Bautista, M ;
Castañón, C ;
Herrera, L ;
Ruano, E ;
Sinay, JJ ;
Sánchez, E ;
Oviedo, GIH ;
Obed, F ;
Salgado, JE ;
Vázquez, JL ;
Baca, M ;
Gutiérrez, M ;
Centella, C ;
Espinosa, J ;
Martínez, D ;
Olmedo, B ;
Espinoza, CEO ;
Núñez, R ;
Haylock, M ;
Benavides, H ;
Mayorga, R .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2005, 110 (D23) :1-15
[2]   Global observed changes in daily climate extremes of temperature and precipitation [J].
Alexander, LV ;
Zhang, X ;
Peterson, TC ;
Caesar, J ;
Gleason, B ;
Tank, AMGK ;
Haylock, M ;
Collins, D ;
Trewin, B ;
Rahimzadeh, F ;
Tagipour, A ;
Kumar, KR ;
Revadekar, J ;
Griffiths, G ;
Vincent, L ;
Stephenson, DB ;
Burn, J ;
Aguilar, E ;
Brunet, M ;
Taylor, M ;
New, M ;
Zhai, P ;
Rusticucci, M ;
Vazquez-Aguirre, JL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D5)
[3]  
[Anonymous], 1973, Nonparametric statistical inference
[4]  
Easterling D.R., 2003, Bull. Am. Meteorol. Soc, V84, P1403, DOI DOI 10.1175/BAMS-84-10-1403
[5]   Maximum and minimum temperature trends for the globe [J].
Easterling, DR ;
Horton, B ;
Jones, PD ;
Peterson, TC ;
Karl, TR ;
Parker, DE ;
Salinger, MJ ;
Razuvayev, V ;
Plummer, N ;
Jamason, P ;
Folland, CK .
SCIENCE, 1997, 277 (5324) :364-367
[6]   Rainfall variability and changes in Southern Africa during the 20th century in the global warming context [J].
Fauchereau, N ;
Trzaska, S ;
Rouault, M ;
Richard, Y .
NATURAL HAZARDS, 2003, 29 (02) :139-154
[7]  
Frei C, 2001, J CLIMATE, V14, P1568, DOI 10.1175/1520-0442(2001)014<1568:DPOTIR>2.0.CO
[8]  
2
[9]   Observed coherent changes in climatic extremes during the second half of the twentieth century [J].
Frich, P ;
Alexander, LV ;
Della-Marta, P ;
Gleason, B ;
Haylock, M ;
Tank, AMGK ;
Peterson, T .
CLIMATE RESEARCH, 2002, 19 (03) :193-212
[10]   Changes in the probability of heavy precipitation: Important indicators of climatic change [J].
Groisman, PY ;
Karl, TR ;
Easterling, DR ;
Knight, RW ;
Jamason, PF ;
Hennessy, KJ ;
Suppiah, R ;
Page, CM ;
Wibig, J ;
Fortuniak, K ;
Razuvaev, VN ;
Douglas, A ;
Forland, E ;
Zhai, PM .
CLIMATIC CHANGE, 1999, 42 (01) :243-283