THE PRINCIPLE OF SPACE-FOR-TIME SUBSTITUTION IN PREDICTING BETULA SPP. BIOMASS CHANGE RELATED TO CLIMATE SHIFTS

被引:0
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作者
Usoltsev, V. A. [2 ,3 ]
Lin, H. [1 ,4 ,5 ,6 ]
Shobairi, S. O. R. [1 ]
Tsepordey, I. S. [3 ]
Ye, Z. [1 ,4 ,5 ,6 ]
Anees, S. A. [7 ]
机构
[1] Cent South Univ Forestry & Technol, Res Ctr Forestry Remote Sensing & Informat Engn, Changsha 410004, Peoples R China
[2] Ural State Forest Engn Univ, Siberian Tract 37, Ekaterinburg 620100, Russia
[3] Russian Acad Sci, Ural Branch, Bot Garden, Ul 8 Marta,202a, Ekaterinburg 620144, Russia
[4] Key Lab Forestry Remote Sensing Based Big Data &, Changsha 410004, Peoples R China
[5] State Forestry Adm Forest Resources Management &, Key Lab, Changsha 410004, Peoples R China
[6] Changsha Changchang Forestry Technol Consulting C, Changsha 410004, Peoples R China
[7] Beijing Forestry Univ, Forestry Coll, Beijing Key Lab Precis Forestry, Beijing 100083, Peoples R China
关键词
hydrothermal gradients; biomass components; allometric models; mean January temperature; annual precipitation; CARBON STORAGE; SILVER FIR; GROWTH; NORTHEASTERN; ALLOMETRY; EQUATIONS; VARIABLES; PATTERNS; TREELINE; MODEL;
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
Human society faces problems of a global scale today, as a result of which the priorities of environmental research are shifting to the macro level, and ecology has entered the era of "big data". The authors have created a database of 1,717 model trees of Betula spp. with measured indicators of diameter at breast height (DBH), tree height, age, and aboveground biomass growing in the territory of Eurasia. Regression models for aboveground biomass components are calculated, including the dendrological indices mentioned, and two climate indicators as independent variables. Based on the theory of space-for time substitution, the obtained patterns of changes in aboveground biomass in the territorial climatic gradients of Eurasia are used to predict changes in biomass due to climate shifts. In accordance with the law of the limiting factor by Liebig, it is established that in sufficiently moisture-rich climatic zones, an increase in temperature by 1??C with a constant amount of precipitation causes an increase in biomass, and in water-deficient zones ??? its decrease. In warm climatic zones, a decrease in precipitation by 100 mm at a constant average January temperature causes a decrease in biomass, and in cold climatic zones ??? its increase.
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页数:16
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