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Climate change, allowable emission, and earth system response to representative concentration pathway scenarios

机译:气候变化,容许排放量和地球系统对代表性浓度路径情景的响应

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摘要

To understand the mechanisms of long-term climate and carbon cycle feedback with anthropogenic impact, past simulations (1850-2005) and projection experiments (2006 to 2100) were conducted using a new Earth system model named "MIROC-ESM", forced by four representative concentration pathway (RCP) scenarios that describe how greenhouse gases (GHGs), aerosols, and land-use will develop in the future. From these projections, temperature rise from 1850 to 2100 ranged from 2.4 K in the RCP2.6 scenario to 6.2 K in the RCP8.5 scenario. We found that there are discrepancies between the RCPs and the estimates of our model in both allowable fossil fuel and land-use change emissions. The former showed systematic discrepancies likely due to strong positive feedbacks in the model, but the latter did not. The likely reason for the difference in land-use emissions is the modeling of land-use change processes or definitions for the emission. Climate response to the increase of atmospheric carbon showed large variation among scenarios, strongly affected by ocean heat uptake efficiency that could depend on the rate of atmospheric CO _2 increase in each scenario. Large variation between scenarios was also found in carbon cycle sensitivity measured by cumulative airborne fraction. The variation in carbon cycle sensitivity may be attributable to the dependence of concentration-carbon feedback on the rate of atmospheric CO _2 increase. The earth system would show a similar response to emitted carbon during the 21st century if the difference of ocean heat uptake efficiency between scenarios were small. The earth system responds to RCP6.0 with less sensitivity to emitted carbon when compared with other scenarios because of high-efficiency carbon uptakes by land and ocean ecosystems. In contrast, RCP2.6 showed high sensitivity of the earth system to carbon emission, and apparently showed different behavior from other scenarios due to early reduction of GHGs.
机译:为了了解长期气候和碳循环反馈对人为影响的机制,过去的模拟(1850-2005年)和投影实验(2006年至2100年)使用了新的地球系统模型“ MIROC-ESM”,由四个代表性的浓缩途径(RCP)场景,描述了未来温室气体(GHG),气溶胶和土地利用的发展方式。根据这些预测,温度从1850年升高到2100年,范围从RCP2.6方案中的2.4 K到RCP8.5方案中的6.2K。我们发现,在允许的化石燃料和土地利用变化排放量方面,RCP与我们模型的估计值之间存在差异。前者显示出系统上的差异,可能是由于模型中存在强烈的积极反馈,而后者则没有。土地利用排放差异的可能原因是对土地利用变化过程或排放定义建模。气候对大气碳增加的响应在各种情景中显示出很大的变化,受海洋热吸收效率的强烈影响,这可能取决于每种情景中大气CO _2的增加速度。通过累积的空气传播分数测量的碳循环敏感性也发现了情景之间的巨大差异。碳循环敏感性的变化可归因于浓度-碳反馈对大气CO _2增加速率的依赖性。如果情景之间的海洋吸热效率差异很小,则地球系统将在21世纪对排放的碳表现出类似的响应。与其他方案相比,地球系统对RCP6.0的响应对碳排放的敏感性较低,这是因为陆地和海洋生态系统对碳的吸收效率很高。相反,RCP2.6显示出地球系统对碳排放的高度敏感性,并且由于温室气体的早期减少,显然表现出与其他情况不同的行为。

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