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气候变化引起的泥炭地植被物候和组成变化对碳平衡的影响。

Impact of climate change-induced alterations in peatland vegetation phenology and composition on carbon balance.

机构信息

Laboratory of Bioclimatology, Department of Ecology and Environmental Protection, Faculty of Environmental Engineering and Mechanical Engineering, Poznan University of Life Sciences, Piątkowska 94, 60-649 Poznań, Poland.

Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, 7500 AE Enschede, the Netherlands.

出版信息

Sci Total Environ. 2022 Jun 25;827:154294. doi: 10.1016/j.scitotenv.2022.154294. Epub 2022 Mar 2.

Abstract

Global climate is changing faster than humankind has ever experienced. Model-based predictions of future climate are becoming more complex and precise, but they still lack crucial information about the reaction of some important ecosystems, such as peatlands. Peatlands belong to one of the largest carbon stores on the Earth. They are mostly distributed in high latitudes, where the temperature rises faster than in the other parts of the planet. Warmer climate and changes in precipitation patterns cause changes in the composition and phenology of peatland vegetation. Peat mosses are becoming less abundant, vascular plants cover is increasing, and the vegetation season and phenophases of vascular plants start sooner. The alterations in vegetation cause changes in the carbon assimilation and release of greenhouse gases. Therefore, this article reviews the impact of climate change-induced alterations in peatland vegetation phenology and composition on future climate and the uncertainties that need to be addressed for more accurate climate prediction.

摘要

全球气候的变化速度超过了人类以往的任何经历。基于模型的未来气候预测变得越来越复杂和精确,但它们仍然缺乏一些重要生态系统(如泥炭地)反应的关键信息。泥炭地属于地球上最大的碳储存库之一。它们主要分布在高纬度地区,那里的温度上升速度比地球上其他地区更快。气候变暖以及降水模式的变化导致泥炭地植被的组成和物候发生变化。泥炭藓的丰度减少,维管植物的覆盖度增加,植被季节和维管植物物候期提前。植被的改变导致温室气体的碳同化和释放发生变化。因此,本文综述了气候变化引起的泥炭地植被物候和组成变化对未来气候的影响,以及为了更准确地进行气候预测需要解决的不确定性。

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