Effects of land-use change on matter and energy exchange between ecosystems in the rain forest margin and the atmosphere

被引:0
|
作者
Ibrom, Andreas [1 ,4 ]
Oltchev, Alexander [1 ,6 ]
June, Tania [2 ,5 ]
Ross, Thomas [1 ]
Kreilein, Heiner [1 ]
Falk, Ulrike [1 ]
Merklein, Johannes [1 ]
Twele, Andre [7 ]
Rakkibu, Golam [1 ]
Grote, Stefan [1 ]
Rauf, Abdul [3 ]
Gravenhorst, Gode [1 ]
机构
[1] Univ Gottingen, Inst Bioclimatol, Busgenweg 2, D-3400 Gottingen, Germany
[2] SEAMEO BIOTROP, Bogor, Indonesia
[3] UNTAD, Palu 94118, Indonesia
[4] Riso Natl Lab, DK-4000 Roskilde, Denmark
[5] Bogor Agr Univ, SEAMEO BIOTROP, Fac Math & Natural Resources, Bogor, Indonesia
[6] Russian Acad Sci, AN Severtsov Inst Ecol & Evolut, Moscow 119071, Russia
[7] Univ Gottingen, GIS and Remote Sensing, Inst Geog, Dept Cartog, D-37077 Gottingen, Germany
来源
STABILITY OF TROPICAL RAINFOREST MARGINS: LINKING ECOLOGICAL, ECONOMIC AND SOCIAL CONSTRAINTS OF LAND USE AND CONSERVATION | 2007年
关键词
land-use change; carbon dioxide fluxes; energy fluxes; montane tropical rain forest; Cacao agroforestry system; eddy correlation; regional modelling; SVAT model; remote sensing;
D O I
暂无
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Greenhouse gas and energy fluxes between the land surface and the atmosphere are important aspects for the evaluation of land-use options in tropical areas. Changes in vegetation cover alter the capacity to absorb carbon dioxide and solar radiation from the atmosphere and influence the magnitudes of latent and sensible heat flows to the atmosphere. If happening at a larger spatial scale, land-use change can lead to significant local feedbacks like drought, flooding, soil erosion or shifts in local climate. Up to now only little was known about how typical ecosystems of the rain forest margin areas interact with the atmosphere. We present here results from a sub-program of STORMA (Stability of rain forest margins in Indonesia, SFB-552-B1), to describe the energy, CO2 and water fluxes between a larger tropical area and the atmosphere. Field measurements with the eddy correlation method showed that a Cacao agroforestry system (AFS) was a small source Of CO2, whereas a tropical rain forest was a strong CO2 sink during the one year observation period. In addition, the rain forest evaporated much more water compared to the Cacao AFS. We applied a series of models to extrapolate the results from the field investigations to the region, including so-called SVAT models of differing complexity, and a simple PAR efficiency model to predict net primary production from regional meteorological and remote sensing data. In all cases, we discovered a large spatial variability in CO2 and water vapour fluxes. We investigated the sensitivity of the models to changes in climatic drivers or land-use parameters from the current to a more intensified agriculture. The selected land-use scenarios reduced carbon dioxide sequestration and total evaporation and increased sensible heat fluxes and thus surface temperatures. We conclude that there is still a lack of field observations to better understand and simulate the behaviour of tropical land-use systems. If the necessary detail on model parameter values, which characterise the differences between the land-use systems, is known, the existing model approaches are suitable to investigate consequences of land-use change to regional biogeochemical cycling, water utilisation and climate change.
引用
收藏
页码:463 / +
页数:6
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