気候の極端さをモデル化する(Modeling climate extremes)

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2023-09-14 オークリッジ国立研究所(ORNL)

◆オークリッジ国立研究所とノーザーストン大学の研究者が、気候変動に伴う極端な気象条件が大気中の炭素吸収に及ぼす影響をモデル化しました。その結果、21世紀末までに地球の88%の地域が炭素排出源になる可能性があることが明らかになりました。
◆これらの極端気象は数か月から数年にわたり、植物の生産性を低下させ、食品や繊維、燃料の生産に影響を及ぼす可能性があります。また、山火事などの出来事も森林に貯蔵された炭素からの排出を引き起こすことがあります。研究は気象条件の複雑な相互作用を包括的に理解するためにモデルを使用し、特に熱帯地域が極端な気象に最も影響を受ける可能性が高いことを指摘しています。

<関連情報>

炭素循環の極端さが21世紀後半の陸域炭素吸収源の弱体化を加速する
Carbon cycle extremes accelerate weakening of the land carbon sink in the late 21st century

Bharat Sharma, Jitendra Kumar, Auroop R. Ganguly, and Forrest M. Hoffman
Biogeosciences  Published:22 May 2023
DOI:https://doi.org/10.5194/bg-20-1829-2023

https://bg.copernicus.org/articles/20/1829/2023/bg-20-1829-2023-f01

Abstract

Increasing surface temperature could lead to enhanced evaporation, reduced soil moisture availability, and more frequent droughts and heat waves. The spatiotemporal co-occurrence of such effects further drives extreme anomalies in vegetation productivity and net land carbon storage. However, the impacts of climate change on extremes in net biospheric production (NBP) over longer time periods are unknown. Using the percentile threshold on the probability distribution curve of NBP anomalies, we computed negative and positive extremes in NBP. Here we show that due to climate warming, about 88 % of global regions will experience a larger magnitude of negative NBP extremes than positive NBP extremes toward the end of 2100, which accelerate the weakening of the land carbon sink. Our analysis indicates the frequency of negative extremes associated with declines in biospheric productivity was larger than positive extremes, especially in the tropics. While the overall impact of warming at high latitudes is expected to increase plant productivity and carbon uptake, high-temperature anomalies increasingly induce negative NBP extremes toward the end of the 21st century. Using regression analysis, we found soil moisture anomalies to be the most dominant individual driver of NBP extremes. The compound effect of hotness, dryness, and fire caused extremes at more than 50 % of the total grid cells. The larger proportion of negative NBP extremes raises a concern about whether the Earth is capable of increasing vegetation production with a growing human population and rising demand for plant material for food, fiber, fuel, and building materials. The increasing proportion of negative NBP extremes highlights the consequences not only of reduction in total carbon uptake capacity but also of conversion of land to a carbon source.

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1702地球物理及び地球化学
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