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首页> 外文期刊>International Journal of Geosciences >How to Heat a Planet? Impact of Anthropogenic Landscapes on Earth’s Albedo and Temperature
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How to Heat a Planet? Impact of Anthropogenic Landscapes on Earth’s Albedo and Temperature

机译:如何加热一个星球?人为景观对地球玻璃玻璃和温度的影响

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摘要

Today anthropogenic climate change is underway and predicted future global temperatures vary significantly. However, the drivers of current climate change and their links to Earth’s natural glacial cycle have yet to be fully resolved. Currently, many on a local level understand, and are exposed to, the heat energy generated by what’s referred to as the urban heat island effect (UHI), whereby natural flora with higher albedos is replaced by manmade urban areas with lower albedos. This heat effect is not constrained to these regions and all anthropogenic surfaces with lower albedos need to be studied and quantified as the accumulated additional heat energy (infrared energy) is trapped within Earth’s atmosphere and could affect the Earth on a planetary level. Deployed satellites have detected critical changes to Earth’s albedo to lower levels, however the cause and impact of these changes have yet to be fully understood and incorporated into Global Circulation models (GCMs). Here it’s shown that industrialization of anthropogenic landscape practices of the past century has displaced millions of square kilometres of naturally high albedo grasslands with lower albedo agricultural landscapes. Utilising a fundamental Energy Balance Model, (EBM) it’s demonstrated these specific changes have generated vast amounts of additional heat energy which is trapped by the atmosphere, transferred and stored within the oceans of the Earth as shown in Figure 1 . The total additional heat energy accumulated over the preceding 110 years correlates to that required to warm the Earth to the levels seen to date, altering Earth’s overall energy budget. This energy will continue to accumulate and warm the Earth to a predicted 1.60 ± 0.20 Celsius by 2050 over 1910 levels. These findings are independent of anthropogenic Greenhouse Gas (GHG) additions and are further validated by predicting Earth’s temperature and albedo at the last glacial maxima, suggesting that an albedo cycle aligned to Gaia theory is the primary driver of Earth’s natural climate cycle.
机译:如今,人为气候变化正在进行中,预测未来的全球气温会显着变化。然而,当前气候变化的驱动因素及其与地球天然冰川周期的联系尚未得到完全解决。目前,许多人在局部层面理解,并暴露于被称为城市热岛效果(UHI)产生的热能,由此与较高的Albedos的天然植物群取代,由Mandade Urban地区替换为较低的Albedos。这种热效应不约束这些区域,并且需要研究和量化具有下层的所有人类表面,并且随着累积的额外热能(红外能量)被捕获在地球大气中并且可能影响地球的行星水平。部署的卫星对地球的反照会进行了危急变化,但这些变化的原因和影响尚未得到完全理解和纳入全局循环模型(GCMS)。在这里,它表明过去世纪的人为景观实践的产业化已经流离了数百万平方公里的自然高的反博德草地,具有较低的反医生农业景观。利用基本能量平衡模型(EBM),它证明了这些特定的变化产生了大量的额外热能,这些热能被大气捕获,转移和储存在地球的海洋内,如 图1所示。在前面的110年中积累的额外热能与将地球加热到迄今为止的水平,改变地球的整体能源预算所需的总热能相关。在1910年,这种能量将继续将地球累积和温暖到预测的1.60±0.20摄氏度。这些发现与人为温室气体(GHG)添加,并通过预测最后的冰川最大值的地球的温度和反玻璃进一步验证,这表明对Gaia理论一致的反照循环是地球自然气候循环的主要驱动因素。

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