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用于估算非洲陆地初级生产力的遥感与动态植被模型之间的比较。

Comparison between remote sensing and a dynamic vegetation model for estimating terrestrial primary production of Africa.

作者信息

Ardö Jonas

机构信息

Department of Physical Geography and Ecosystem Science, Lund University, Sölvegatan 12, Lund, 223-62 Sweden.

出版信息

Carbon Balance Manag. 2015 Mar 31;10:8. doi: 10.1186/s13021-015-0018-5. eCollection 2015 Dec.

DOI:10.1186/s13021-015-0018-5
PMID:25960765
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC4412648/
Abstract

BACKGROUND

Africa is an important part of the global carbon cycle. It is also a continent facing potential problems due to increasing resource demand in combination with climate change-induced changes in resource supply. Quantifying the pools and fluxes constituting the terrestrial African carbon cycle is a challenge, because of uncertainties in meteorological driver data, lack of validation data, and potentially uncertain representation of important processes in major ecosystems. In this paper, terrestrial primary production estimates derived from remote sensing and a dynamic vegetation model are compared and quantified for major African land cover types.

RESULTS

Continental gross primary production estimates derived from remote sensing were higher than corresponding estimates derived from a dynamic vegetation model. However, estimates of continental net primary production from remote sensing were lower than corresponding estimates from the dynamic vegetation model. Variation was found among land cover classes, and the largest differences in gross primary production were found in the evergreen broadleaf forest. Average carbon use efficiency (NPP/GPP) was 0.58 for the vegetation model and 0.46 for the remote sensing method. Validation versus in situ data of aboveground net primary production revealed significant positive relationships for both methods. A combination of the remote sensing method with the dynamic vegetation model did not strongly affect this relationship.

CONCLUSION

Observed significant differences in estimated vegetation productivity may have several causes, including model design and temperature sensitivity. Differences in carbon use efficiency reflect underlying model assumptions. Integrating the realistic process representation of dynamic vegetation models with the high resolution observational strength of remote sensing may support realistic estimation of components of the carbon cycle and enhance resource monitoring, providing suitable validation data is available.

摘要

背景

非洲是全球碳循环的重要组成部分。由于资源需求不断增加,再加上气候变化导致资源供应发生变化,非洲大陆面临着潜在问题。由于气象驱动数据存在不确定性、缺乏验证数据以及主要生态系统中重要过程的代表性可能存在不确定性,因此量化构成非洲陆地碳循环的碳库和通量是一项挑战。在本文中,对源自遥感和动态植被模型的非洲主要土地覆盖类型的陆地初级生产估计值进行了比较和量化。

结果

源自遥感的大陆总初级生产估计值高于源自动态植被模型的相应估计值。然而,源自遥感的大陆净初级生产估计值低于动态植被模型的相应估计值。在土地覆盖类别之间发现了差异,常绿阔叶林的总初级生产差异最大。植被模型的平均碳利用效率(NPP/GPP)为0.58,遥感方法为0.46。与地上净初级生产的原位数据进行验证,结果表明两种方法均存在显著的正相关关系。遥感方法与动态植被模型的结合并未强烈影响这种关系。

结论

观察到的估计植被生产力的显著差异可能有多种原因,包括模型设计和温度敏感性。碳利用效率的差异反映了潜在的模型假设。将动态植被模型的现实过程表示与遥感的高分辨率观测优势相结合,可能有助于对碳循环组成部分进行现实估计并加强资源监测,前提是有合适的验证数据。

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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/c1f5fb3ef391/13021_2015_18_Fig1_HTML.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/189aa4cd7431/13021_2015_18_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/07a323ffcc8a/13021_2015_18_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/cff6ff3d428e/13021_2015_18_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/a61930efda3d/13021_2015_18_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/212dcb8b9be2/13021_2015_18_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/d4dede49e904/13021_2015_18_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5d3e/5256540/58fb60038b79/13021_2015_18_Fig10_HTML.jpg

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本文引用的文献

1
Effects of Climate Change on Plant Respiration.气候变化对植物呼吸作用的影响。
Ecol Appl. 1991 May;1(2):157-167. doi: 10.2307/1941808.
2
Drought impact on forest carbon dynamics and fluxes in Amazonia.干旱对亚马逊地区森林碳动态和通量的影响。
Nature. 2015 Mar 5;519(7541):78-82. doi: 10.1038/nature14213.
3
Emergent global patterns of ecosystem structure and function from a mechanistic general ecosystem model.基于机理通用生态系统模型的生态系统结构与功能的全球涌现模式
基于经验模型与轻度利用效率模型估算废弃喀斯特草地演替中期生态系统碳通量
PLoS One. 2020 Aug 7;15(8):e0237351. doi: 10.1371/journal.pone.0237351. eCollection 2020.
4
The impact of increasing land productivity on groundwater dynamics: a case study of an oasis located at the edge of the Gobi Desert.土地生产力提高对地下水动态的影响:以戈壁沙漠边缘的一个绿洲为例
Carbon Balance Manag. 2020 May 2;15(1):7. doi: 10.1186/s13021-020-00142-7.
5
Effect of climate dataset selection on simulations of terrestrial GPP: Highest uncertainty for tropical regions.气候数据集选择对陆地总初级生产力模拟的影响:热带地区不确定性最高。
PLoS One. 2018 Jun 21;13(6):e0199383. doi: 10.1371/journal.pone.0199383. eCollection 2018.
6
Towards the co-ordination of terrestrial ecosystem protocols across European research infrastructures.迈向欧洲研究基础设施间陆地生态系统协议的协调。
Ecol Evol. 2017 Apr 23;7(11):3967-3975. doi: 10.1002/ece3.2997. eCollection 2017 Jun.
7
The global impact factors of net primary production in different land cover types from 2005 to 2011.2005年至2011年不同土地覆盖类型净初级生产力的全球影响因素。
Springerplus. 2016 Aug 2;5(1):1235. doi: 10.1186/s40064-016-2910-1. eCollection 2016.
PLoS Biol. 2014 Apr 22;12(4):e1001841. doi: 10.1371/journal.pbio.1001841. eCollection 2014 Apr.
4
Variations in atmospheric CO2 growth rates coupled with tropical temperature.大气 CO2 增长率的变化与热带温度有关。
Proc Natl Acad Sci U S A. 2013 Aug 6;110(32):13061-6. doi: 10.1073/pnas.1219683110. Epub 2013 Jul 24.
5
African tropical rainforest net carbon dioxide fluxes in the twentieth century.20 世纪非洲热带雨林净二氧化碳通量。
Philos Trans R Soc Lond B Biol Sci. 2013 Jul 22;368(1625):20120376. doi: 10.1098/rstb.2012.0376. Print 2013.
6
Evaluation of terrestrial carbon cycle models for their response to climate variability and to CO2 trends.评估陆地碳循环模型对气候变化和 CO2 趋势的响应。
Glob Chang Biol. 2013 Jul;19(7):2117-32. doi: 10.1111/gcb.12187. Epub 2013 Apr 3.
7
Increase in observed net carbon dioxide uptake by land and oceans during the past 50 years.过去 50 年来,陆地和海洋观测到的净二氧化碳吸收量增加。
Nature. 2012 Aug 2;488(7409):70-2. doi: 10.1038/nature11299.
8
Comment on "Drought-induced reduction in global terrestrial net primary production from 2000 through 2009".评论“2000 年至 2009 年干旱导致的全球陆地净初级生产力减少”。
Science. 2011 Aug 26;333(6046):1093; author reply 1093. doi: 10.1126/science.1199048.
9
Comment on "Drought-induced reduction in global terrestrial net primary production from 2000 through 2009".评论“2000 年至 2009 年干旱导致的全球陆地净初级生产力减少”。
Science. 2011 Aug 26;333(6046):1093; author reply 1093. doi: 10.1126/science.1199544.
10
The carbon balance of Africa: synthesis of recent research studies.非洲碳平衡:近期研究综述。
Philos Trans A Math Phys Eng Sci. 2011 May 28;369(1943):2038-57. doi: 10.1098/rsta.2010.0328.