A projection of severe near-surface permafrost degradation during the 21st century

被引:343
作者
Lawrence, DM
Slater, AG
机构
[1] Natl Ctr Atmospher Res, Climate & Global Dynam Div, Boulder, CO 80307 USA
[2] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
关键词
D O I
10.1029/2005GL025080
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The current distribution and future projections of permafrost are examined in a fully coupled global climate model, the Community Climate System Model, version 3 (CCSM3) with explicit treatment of frozen soil processes. The spatial extent of simulated present-day permafrost in CCSM3 agrees well with observational estimates - an area, excluding ice sheets, of 10.5 million km(2). By 2100, as little as 1.0 million km(2) of near-surface permafrost remains. Freshwater discharge to the Arctic Ocean rises by 28% over the same period, largely due to increases in precipitation that outpace increases in evaporation, with about 15% of the rise directly attributable to melting ground ice. Such large changes in permafrost may provoke feedbacks such as activation of the soil carbon pool and a northward expansion of shrubs and forests.
引用
收藏
页码:1 / 5
页数:5
相关论文
共 29 条
[1]   Permafrost zonation and climate change in the northern hemisphere: Results from transient general circulation models [J].
Anisimov, OA ;
Nelson, FE .
CLIMATIC CHANGE, 1997, 35 (02) :241-258
[2]   Implications of climate change for freshwater inflows to the Arctic Ocean [J].
Arnell, NW .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2005, 110 (D7) :1-9
[3]   Offset of the potential carbon sink from boreal forestation by decreases in surface albedo [J].
Betts, RA .
NATURE, 2000, 408 (6809) :187-190
[4]  
BRANSTETTER ML, 1999, 14 C HYDR AM MET SOC
[5]   Role of land-surface changes in Arctic summer warming [J].
Chapin, FS ;
Sturm, M ;
Serreze, MC ;
McFadden, JP ;
Key, JR ;
Lloyd, AH ;
McGuire, AD ;
Rupp, TS ;
Lynch, AH ;
Schimel, JP ;
Beringer, J ;
Chapman, WL ;
Epstein, HE ;
Euskirchen, ES ;
Hinzman, LD ;
Jia, G ;
Ping, CL ;
Tape, KD ;
Thompson, CDC ;
Walker, DA ;
Welker, JM .
SCIENCE, 2005, 310 (5748) :657-660
[6]   Thawing sub-arctic permafrost:: Effects on vegetation and methane emissions -: art. no. L04501 [J].
Christensen, TR ;
Johansson, TR ;
Åkerman, HJ ;
Mastepanov, M ;
Malmer, N ;
Friborg, T ;
Crill, P ;
Svensson, BH .
GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (04) :L045011-4
[7]  
COLLINS WD, 2005, IN PRESS J CLIM
[8]  
Dai A, 2002, J HYDROMETEOROL, V3, P660, DOI 10.1175/1525-7541(2002)003<0660:EOFDFC>2.0.CO
[9]  
2
[10]   Sensitivity of boreal forest carbon balance to soil thaw [J].
Goulden, ML ;
Wofsy, SC ;
Harden, JW ;
Trumbore, SE ;
Crill, PM ;
Gower, ST ;
Fries, T ;
Daube, BC ;
Fan, SM ;
Sutton, DJ ;
Bazzaz, A ;
Munger, JW .
SCIENCE, 1998, 279 (5348) :214-217