High chance that current atmospheric greenhouse concentrations commit to warmings greater than 1.5°C over land

被引:32
作者
Huntingford, Chris [1 ]
Mercado, Lina M. [1 ,2 ]
机构
[1] Ctr Ecol & Hydrol, Wallingford OX10 8BB, Oxon, England
[2] Univ Exeter, Coll Life & Environm Sci, Amory Bldg,Rennes Dr, Exeter EX4 4RJ, Devon, England
关键词
CLIMATE-CHANGE; COLD-SEASON; MODEL; EMISSIONS; CO2;
D O I
10.1038/srep30294
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The recent Paris UNFCCC climate meeting discussed the possibility of limiting global warming to 2 degrees C since pre-industrial times, or possibly even 1.5 degrees C, which would require major future emissions reductions. However, even if climate is stabilised at current atmospheric greenhouse gas (GHG) concentrations, those warming targets would almost certainly be surpassed in the context of mean temperature increases over land only. The reason for this is two-fold. First, current transient warming lags significantly below equilibrium or "committed" warming. Second, almost all climate models indicate warming rates over land are much higher than those for the oceans. We demonstrate this potential for high eventual temperatures over land, even for contemporary GHG levels, using a large set of climate models and for which climate sensitivities are known. Such additional land warming has implications for impacts on terrestrial ecosystems and human well-being. This suggests that even if massive and near-immediate emissions reductions occur such that atmospheric GHGs increase further by only small amounts, careful planning is needed by society to prepare for higher land temperatures in an eventual equilibrium climatic state.
引用
收藏
页数:7
相关论文
共 27 条
[11]   Enhanced cold-season warming in semi-arid regions [J].
Huang, J. ;
Guan, X. ;
Ji, F. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2012, 12 (12) :5391-5398
[12]   1.5 °C and climate research after the Paris Agreement [J].
Hulme, Mike .
NATURE CLIMATE CHANGE, 2016, 6 (03) :222-224
[13]   An analogue model to derive additional climate change scenarios from existing GCM simulations [J].
Huntingford, C ;
Cox, PM .
CLIMATE DYNAMICS, 2000, 16 (08) :575-586
[14]   IMOGEN: an intermediate complexity model to evaluate terrestrial impacts of a changing climate [J].
Huntingford, C. ;
Booth, B. B. B. ;
Sitch, S. ;
Gedney, N. ;
Lowe, J. A. ;
Liddicoat, S. K. ;
Mercado, L. M. ;
Best, M. J. ;
Weedon, G. P. ;
Fisher, R. A. ;
Lomas, M. R. ;
Good, P. ;
Zelazowski, P. ;
Everitt, A. C. ;
Spessa, A. C. ;
Jones, C. D. .
GEOSCIENTIFIC MODEL DEVELOPMENT, 2010, 3 (02) :679-687
[15]   The link between a global 2°C warming threshold and emissions in years 2020, 2050 and beyond [J].
Huntingford, Chris ;
Lowe, Jason A. ;
Gohar, Laila K. ;
Bowerman, Niel H. A. ;
Allen, Myles R. ;
Raper, Sarah C. B. ;
Smith, Stephen M. .
ENVIRONMENTAL RESEARCH LETTERS, 2012, 7 (01)
[16]  
Ji F, 2014, NAT CLIM CHANGE, V4, P462, DOI [10.1038/NCLIMATE2223, 10.1038/nclimate2223]
[17]   An explanation for the difference between twentieth and twenty-first century land-sea warming ratio in climate models [J].
Joshi, M. M. ;
Lambert, F. H. ;
Webb, M. J. .
CLIMATE DYNAMICS, 2013, 41 (7-8) :1853-1869
[18]   The Relationship between Land-Ocean Surface Temperature Contrast and Radiative Forcing [J].
Lambert, F. Hugo ;
Webb, Mark J. ;
Joshi, Manoj M. .
JOURNAL OF CLIMATE, 2011, 24 (13) :3239-3256
[19]   How difficult is it to recover from dangerous levels of global warming? [J].
Lowe, J. A. ;
Huntingford, C. ;
Raper, S. C. B. ;
Jones, C. D. ;
Liddicoat, S. K. ;
Gohar, L. K. .
ENVIRONMENTAL RESEARCH LETTERS, 2009, 4 (01)
[20]  
MANABE S, 1991, J CLIMATE, V4, P785, DOI 10.1175/1520-0442(1991)004<0785:TROACO>2.0.CO