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Sources or sinks? The responses of tropical forests to current and future climate and atmospheric composition.

机译:源还是汇?热带森林对当前和未来气候以及大气成分的响应。

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摘要

How tropical rainforests are responding to the ongoing global changes in atmospheric composition and climate is little studied and poorly understood. Although rising atmospheric carbon dioxide (CO2) could enhance forest productivity, increased temperatures and drought are likely to diminish it. The limited field data have produced conflicting views of the net impacts of these changes so far. One set of studies has seemed to point to enhanced carbon uptake; however, questions have arisen about these findings, and recent experiments with tropical forest trees indicate carbon saturation of canopy leaves and no biomass increase under enhanced CO2. Other field observations indicate decreased forest productivity and increased tree mortality in recent years of peak temperatures and drought (strong El Niño episodes). To determine current climatic responses of forests around the world tropics will require careful annual monitoring of ecosystem performance in representative forests. To develop the necessary process-level understanding of these responses will require intensified experimentation at the whole-tree and stand levels. Finally, a more complete understanding of tropical rainforest carbon cycling is needed for determining whether these ecosystems are carbon sinks or sources now, and how this status might change during the next century.
机译:关于热带雨林如何对全球不断变化的大气成分和气候做出反应,对此的研究很少,人们对此知之甚少。尽管大气中二氧化碳(CO2)的增加可以提高森林的生产力,但温度升高和干旱可能会减少森林的生产力。迄今为止,有限的现场数据对这些变化的净影响产生了相互矛盾的看法。一组研究似乎表明碳吸收增加。然而,有关这些发现的问题出现了,最近对热带林木进行的实验表明,冠层叶片的碳饱和度很高,并且在二氧化碳增加的情况下生物量没有增加。其他实地观察表明,近年来峰值温度和干旱(强烈的厄尔尼诺现象)导致森林生产力下降和树木死亡率增加。为了确定世界热带地区森林的当前气候响应,将需要每年对代表性森林中的生态系统性能进行仔细的监测。为了对这些响应形成必要的过程级别的理解,将需要在整个树和立场级别上进行更多的实验。最后,需要对热带雨林的碳循环有一个更全面的了解,以确定这些生态系统现在是碳汇还是碳汇,以及这种状况在下一世纪将如何改变。

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