An objective methodology for potential vegetation reconstruction constrained by climate

被引:7
作者
Levavasseur, G. [1 ]
Vrac, M. [1 ]
Roche, D. M. [1 ,2 ]
Paillard, D. [1 ]
Guiot, J. [3 ]
机构
[1] Ctr Etud Saclay, IPSL CEA CNRS INSU UVSQ, UMR 8212, Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France
[2] Vrije Univ Amsterdam, Fac Earth & Life Sci, Dept Earth Sci, Sect Climate Change & Landscape Dynam, NL-1081 HV Amsterdam, Netherlands
[3] Aix Marseille Univ, CNRS, UMR 6635, Ctr Europeen Rech & Enseignement Geosci Environm, F-13545 Aix En Provence 4, France
关键词
statistical modelling; potential; vegetation; multinomial logistic regression; biomes; Westem Europe; climate; LAST GLACIAL MAXIMUM; GLOBAL LAND-COVER; LOGISTIC-REGRESSION; ARCTIC ECOSYSTEMS; POLLEN DATA; YR BP; MODEL; MIDHOLOCENE; EUROPE; BIOMES;
D O I
10.1016/j.gloplacha.2013.01.008
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Reconstructions of modern Potential Natural Vegetation (PNV) are widely used in climate modelling and vegetation survey as a starting point for studies (historical changes of land-use, past or future vegetation distribution modelling, etc.). A PNV distribution is often related to vegetation models, which are based on empirical relationships between vegetation (or pollen data in paleoecological studies) and climate. Vegetation models are used to directly simulate a PNV distribution or to correct vegetation types derived from remotely-sensed observations in human-impacted regions. Consequently, these methods are quite subjective and include biases from models. This article proposes a new approach to build a high-resolution PNV map using a statistical model. As vegetation is a nominal variable, our method consists in applying a multinomial logistic regression (MLR). MLR build statistical relationships between BIOME 6000 data covering Europe and several climatological variables from the Climate Research Unit (CRU). The PNV reconstructed by MLR appears similar to those reconstructed from remotely-sensed data or simulated by a vegetation model (BIOME 4) except in southern Europe with the establishment of warm-temperate forests. MLR produces a realistic PNV distribution, which is the closest to BIOME 6000 data and provides the vegetation distribution in each grid-cell of our map. Moreover, MLR allows us to compute an uncertainty index that appears as a convenient tool to highlight the regions lacking some data toimprove the PNV distribution. The MLR method does not suffer any dynamic biases or subjective corrections and is a fast and objective alternative to the other methods. MLR provides an independent reference for vegetation models that is entirely based on vegetation and climatological data. (C) 2013 Published by Elsevier B.V.
引用
收藏
页码:7 / 22
页数:16
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