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评估阿拉斯加的历史和预测碳平衡:结果综合与政策/管理启示。

Assessing historical and projected carbon balance of Alaska: A synthesis of results and policy/management implications.

机构信息

U.S. Geological Survey, Alaska Cooperative Fish and Wildlife Research Unit, University of Alaska Fairbanks, Fairbanks, Alaska, 99775, USA.

Institute of Arctic Biology, University of Alaska Fairbanks, Fairbanks, Alaska, 99775, USA.

出版信息

Ecol Appl. 2018 Sep;28(6):1396-1412. doi: 10.1002/eap.1768. Epub 2018 Jul 30.

Abstract

We summarize the results of a recent interagency assessment of land carbon dynamics in Alaska, in which carbon dynamics were estimated for all major terrestrial and aquatic ecosystems for the historical period (1950-2009) and a projection period (2010-2099). Between 1950 and 2009, upland and wetland (i.e., terrestrial) ecosystems of the state gained 0.4 Tg C/yr (0.1% of net primary production, NPP), resulting in a cumulative greenhouse gas radiative forcing of 1.68 × 10  W/m . The change in carbon storage is spatially variable with the region of the Northwest Boreal Landscape Conservation Cooperative (LCC) losing carbon because of fire disturbance. The combined carbon transport via various pathways through inland aquatic ecosystems of Alaska was estimated to be 41.3 Tg C/yr (17% of terrestrial NPP). During the projection period (2010-2099), carbon storage of terrestrial ecosystems of Alaska was projected to increase (22.5-70.0 Tg C/yr), primarily because of NPP increases of 10-30% associated with responses to rising atmospheric CO , increased nitrogen cycling, and longer growing seasons. Although carbon emissions to the atmosphere from wildfire and wetland CH were projected to increase for all of the climate projections, the increases in NPP more than compensated for those losses at the statewide level. Carbon dynamics of terrestrial ecosystems continue to warm the climate for four of the six future projections and cool the climate for only one of the projections. The attribution analyses we conducted indicated that the response of NPP in terrestrial ecosystems to rising atmospheric CO (~5% per 100 ppmv CO ) saturates as CO increases (between approximately +150 and +450 ppmv among projections). This response, along with the expectation that permafrost thaw would be much greater and release large quantities of permafrost carbon after 2100, suggests that projected carbon gains in terrestrial ecosystems of Alaska may not be sustained. From a national perspective, inclusion of all of Alaska in greenhouse gas inventory reports would ensure better accounting of the overall greenhouse gas balance of the nation and provide a foundation for considering mitigation activities in areas that are accessible enough to support substantive deployment.

摘要

我们总结了最近一次阿拉斯加陆地碳动态的机构间评估结果,该评估对历史时期(1950-2009 年)和预测时期(2010-2099 年)的所有主要陆地和水生生态系统的碳动态进行了估计。在 1950 年至 2009 年期间,该州的旱地和湿地(即陆地)生态系统每年增加 0.4 太吨碳(占净初级生产力的 0.1%),导致温室气体辐射强迫累计增加 1.68×10 ² W/m²。碳储存的变化在空间上是可变的,因为西北北方景观保护合作组织(LCC)的一个地区由于火灾干扰而失去了碳。通过阿拉斯加内陆水生生态系统的各种途径进行的碳运输总量估计为每年 41.3 太吨碳(占陆地 NPP 的 17%)。在预测期(2010-2099 年),预计阿拉斯加陆地生态系统的碳储存将增加(每年 22.5-70.0 太吨碳),主要是因为与大气 CO ²上升相关的 NPP 增加了 10-30%,氮循环增加,生长季节延长。尽管所有气候预测都预计野火和湿地 CH 向大气排放的碳会增加,但 NPP 的增加足以弥补全州范围内的这些损失。陆地生态系统的碳动态继续为未来六个预测中的四个加热气候,仅为一个预测冷却气候。我们进行的归因分析表明,陆地生态系统中 NPP 对大气中 CO ²的响应在 CO ²增加时达到饱和(在预测中,约在+150 和+450 ppmv 之间)。这种响应,以及对永久冻土解冻的预期,将在 2100 年后更大,并释放大量永久冻土碳,这表明阿拉斯加陆地生态系统的预期碳收益可能无法持续。从国家角度来看,将整个阿拉斯加纳入温室气体清单报告将确保更好地核算国家温室气体总体收支平衡,并为考虑在可进行实质性部署的地区开展缓解活动提供基础。

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