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Abrupt climate change 总被引:4,自引:0,他引:4
Alley RB Marotzke J Nordhaus WD Overpeck JT Peteet DM Pielke RA Pierrehumbert RT Rhines PB Stocker TF Talley LD Wallace JM 《Science (New York, N.Y.)》2003,299(5615):2005-2010
Large, abrupt, and widespread climate changes with major impacts have occurred repeatedly in the past, when the Earth system was forced across thresholds. Although abrupt climate changes can occur for many reasons, it is conceivable that human forcing of climate change is increasing the probability of large, abrupt events. Were such an event to recur, the economic and ecological impacts could be large and potentially serious. Unpredictability exhibited near climate thresholds in simple models shows that some uncertainty will always be associated with projections. In light of these uncertainties, policy-makers should consider expanding research into abrupt climate change, improving monitoring systems, and taking actions designed to enhance the adaptability and resilience of ecosystems and economies. 相似文献
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The climate change commitment 总被引:2,自引:0,他引:2
Wigley TM 《Science (New York, N.Y.)》2005,307(5716):1766-1769
Even if atmospheric composition were fixed today, global-mean temperature and sea level rise would continue due to oceanic thermal inertia. These constant-composition (CC) commitments and their uncertainties are quantified. Constant-emissions (CE) commitments are also considered. The CC warming commitment could exceed 1 degrees C. The CE warming commitment is 2 degrees to 6 degrees C by the year 2400. For sea level rise, the CC commitment is 10 centimeters per century (extreme range approximately 1 to 30 centimeters per century) and the CE commitment is 25 centimeters per century (7 to 50 centimeters per century). Avoiding these changes requires, eventually, a reduction in emissions to substantially below present levels. For sea level rise, a substantial long-term commitment may be impossible to avoid. 相似文献
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Modern global climate change 总被引:5,自引:0,他引:5
Modern climate change is dominated by human influences, which are now large enough to exceed the bounds of natural variability. The main source of global climate change is human-induced changes in atmospheric composition. These perturbations primarily result from emissions associated with energy use, but on local and regional scales, urbanization and land use changes are also important. Although there has been progress in monitoring and understanding climate change, there remain many scientific, technical, and institutional impediments to precisely planning for, adapting to, and mitigating the effects of climate change. There is still considerable uncertainty about the rates of change that can be expected, but it is clear that these changes will be increasingly manifested in important and tangible ways, such as changes in extremes of temperature and precipitation, decreases in seasonal and perennial snow and ice extent, and sea level rise. Anthropogenic climate change is now likely to continue for many centuries. We are venturing into the unknown with climate, and its associated impacts could be quite disruptive. 相似文献
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Australian Academy of Sciences;Royal Flemish Academy of Belgium for Sciences the Arts;Brazilian Academy of Sciences;Royal Society of Canada;Caribbean Academy of Sciences;Chinese Academy of Sciences;French Academy of Sciences;German Academy of Natural Scientists Leopoldina;Indian National Science Academy;Indonesian Academy of Sciences;Royal Irish Academy;Accademia Nazionale dei Lincei 《Science (New York, N.Y.)》2001,292(5520):1261
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Livingstone DA 《Science (New York, N.Y.)》2003,301(5632):468-469
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A continuous 48,000-year-long paleoecological record from Neotropical lower montane forest reveals a consistent forest presence and an ice-age cooling of approximately 5 degrees to 9 degrees C. After 30,000 years of compositional stability, a steady turnover of species marks the 8000-year-long transition from ice-age to Holocene conditions. Although the changes were directional, the rates of community change were no different during this transitional period than in the preceding 30,000-year period of community stability. The warming rate of about 1 degrees C per millennium during the Pleistocene-Holocene transition was an order of magnitude less than the projected changes for the 21st century. 相似文献
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Wiener JB Stewart RB Hammitt JK Hourcade JC 《Science (New York, N.Y.)》2006,311(5759):335-6; author reply 335-6
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Amazon deforestation and climate change 总被引:4,自引:0,他引:4
A coupled numerical model of the global atmosphere and biosphere has been used to assess the effects of Amazon deforestation on the regional and global climate. When the tropical forests in the model were replaced by degraded grass (pasture), there was a significant increase in surface temperature and a decrease in evapotranspiration and precipitation over Amazonia. In the simulation, the length of the dry season also increased; such an increase could make reestablishment of the tropical forests after massive deforestation particularly difficult. 相似文献