陆地碳循环的当前观点

IF 2.3 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
J. Lloyd
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引用次数: 34

摘要

在过去5年左右的时间里,在了解陆地生物圈在全球碳循环中的当前作用方面取得了重大进展,特别是在了解碳库和通量如何受到气候变化(包括年际变率以及较长期气候变化)、大气CO 2浓度增加和大气氮沉积速率变化的影响方面。与此同时,在直接测量生态系统生产力和了解调节陆地系统碳通量的关键潜在机制方面取得了重大进展。本文的主题是对这些进展的简要概述。DOI: 10.1034 / j.1600-0889.1999.00016.x
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Current perspectives on the terrestrial carbon cycle
Over the last 5 or so years, there have been significant advances in the understanding of the current role of the terrestrial biosphere in the global carbon cycle, especially in terms of how pools and fluxes are affected by variations in climate (including interannual variability as well as longer-term climate change), increases in atmospheric CO 2 concentrations and changed rates of atmospheric nitrogen deposition. At the same time, significant advances have been made in terms of both direct measurement of ecosystem productivity and in an understanding of the key underlying mechanisms modulating carbon fluxes from terrestrial systems. A brief synopsis of these advances is the subject of this paper. DOI: 10.1034/j.1600-0889.1999.00016.x
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来源期刊
自引率
0.00%
发文量
3
期刊介绍: Tellus B: Chemical and Physical Meteorology along with its sister journal Tellus A: Dynamic Meteorology and Oceanography, are the international, peer-reviewed journals of the International Meteorological Institute in Stockholm, an independent non-for-profit body integrated into the Department of Meteorology at the Faculty of Sciences of Stockholm University, Sweden. Aiming to promote the exchange of knowledge about meteorology from across a range of scientific sub-disciplines, the two journals serve an international community of researchers, policy makers, managers, media and the general public.
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