Albedo Changes Drive 4.9 to 9.4C Global Warming by 2400

G. Fry
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Abstract

This study ties increasing climate feedbacks to projected warming consistent with temperatures when Earth last had this much CO2 in the air. The relationship between CO2 and temperature in a Vostok ice core is used to extrapolate temperature effects of today’s CO2 levels. The results suggest long-run equilibrium global surface temperatures (GSTs) 5 degrees Celsius warmer than immediately "pre-industrial" (1880). The relationship derived holds well for warmer conditions 4 and 14 million years ago (Mya). Adding CH4 data from Vostok yields 8.5 degrees Celsius warming due to today’s CO2 and CH4 levels. Long-run climate sensitivity to doubled CO2, given Earth’s current ice state, is estimated to be 8.2 degrees Celsius: 1.8 directly from CO2 and 6.4 from albedo effects. Based on the Vostok equation using CO2 only, holding change in GST to 2 degrees Celsius requires 318 ppm CO2. This means Earth’s remaining carbon budget is estimated to be negative 313 billion tonnes. Meeting this target will require very large-scale CO2 removal. Lagged warming of 4.0 degrees Celsius (or 7.4 when CH4 is included), starting from today’s 1.1 degree Celsius change in GST, comes mostly from albedo changes. Their effects are estimated here for ice, snow, sulfates, and cloud cover. This study estimates magnitudes for sulfates and for future snow changes. Magnitudes for ice, cloud cover, and past snow changes are drawn from the literature. Albedo changes, plus their water vapor multiplier, caused an estimated 39 percent of observed GST warming over 1975-2016. Estimated warming effects on GST by water vapor; ocean heat; and net natural carbon emissions (from permafrost, etc.), all drawn from the literature, are included in projections alongside ice, snow, sulfates, and clouds. Six scenarios embody these effects. Projected change in GSTs on land by 2400 range from 2.4 to 9.4 degrees Celsius. Phasing out fossil fuels by 2050 yields 7.1. Ending fossil fuel use immediately yields 4.9, similar to the 5.1 inferred from paleoclimate studies for current CO2 levels. Fossil fuel phase-out by 2050 coupled with removing 71 percent of CO2 emitted to date yields 2.4 degrees Celsius. At the other extreme, postponing peak fossil fuel use to 2035 yields 9.4 degrees Celsius GST, with more warming after 2400.
到2400年,反照率变化将导致全球变暖4.9至9.4摄氏度
这项研究将不断增加的气候反馈与预测的变暖联系起来,与地球上一次空气中有这么多二氧化碳的温度一致。沃斯托克冰芯中二氧化碳和温度之间的关系被用来推断当今二氧化碳水平对温度的影响。结果表明,长期平衡全球表面温度(GSTs)比立即“工业化前”(1880年)高5摄氏度。这一关系适用于400万至1400万年前的温暖环境。加上来自Vostok的CH4数据,由于今天的二氧化碳和CH4水平,气温上升了8.5摄氏度。考虑到地球目前的冰状态,长期气候对二氧化碳的敏感度估计为8.2摄氏度:1.8摄氏度直接来自二氧化碳,6.4摄氏度来自反照率效应。根据仅使用二氧化碳的Vostok方程,将GST的变化保持在2摄氏度需要318ppm的二氧化碳。这意味着地球剩余的碳预算估计为负3130亿吨。要实现这一目标,将需要非常大规模的二氧化碳去除。从今天的1.1摄氏度的GST变化开始,4.0摄氏度的滞后变暖(如果包括CH4,则为7.4摄氏度)主要来自反照率的变化。这里估计了它们对冰、雪、硫酸盐和云层的影响。这项研究估计了硫酸盐和未来积雪变化的量级。冰、云量和过去积雪变化的量级是从文献中得出的。反照率的变化,加上它们的水蒸气乘数,造成了1975-2016年观测到的39%的GST变暖。估计水蒸气对商品及服务税的变暖效应;海洋热;从文献中提取的净自然碳排放量(来自永久冻土等)与冰、雪、硫酸盐和云一起被包括在预测中。六个场景体现了这些影响。预计到2400年,陆上商品及服务税的变化幅度在2.4至9.4摄氏度之间。到2050年逐步淘汰化石燃料的比例为7.1。停止使用化石燃料立即产生4.9,类似于古气候研究对当前二氧化碳水平推断出的5.1。到2050年逐步淘汰化石燃料,再加上迄今为止减少71%的二氧化碳排放,将产生2.4摄氏度的温室效应。在另一种极端情况下,将化石燃料的峰值使用推迟到2035年,将产生9.4摄氏度的GST, 2400年之后将进一步升温。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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