Testing a climato-topographic index for predicting wetlands distribution along an European climate gradient

被引:81
作者
Merot, P
Squividant, H
Aurousseau, P
Hefting, M
Burt, T
Maitre, V
Kruk, M
Butturini, A
Thenail, C
Viaud, V
机构
[1] UMR INRA, ENSA Sol Agron Spatialisat, F-35042 Rennes, France
[2] Univ Utrecht, Dept Plant Ecol & Evolutionary Biol, NL-3508 TB Utrecht, Netherlands
[3] Univ Durham, Dept Geog, Durham DH1 3LE, England
[4] Ecole Polytech Fed Lausanne, Geol Lab, CH-1015 Lausanne, Switzerland
[5] Univ Warmia & Mazury, Dept Ecol & Hydrobiol, PL-10957 Olztyn, Poland
[6] Univ Barcelona, Fac Biol, Dept Ecol, E-08028 Barcelona, Spain
[7] INRA, Unite SAD Armor, F-35042 Rennes, France
关键词
wetland; topographic index; Europe;
D O I
10.1016/S0304-3800(02)00387-3
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Knowledge of the-spatial distribution of wetlands within landscapes is needed for a number of different purposes as non-point pollution control, aquatic life, flood protection or sediment traps or sources. The purpose of this paper was to propose and to test a parsimonious method for predicting wetlands in small catchments across a wide range of geological, topographic and climatic conditions. A climato-topographic index has been derived from the topographic index-taking into account the local slope and the upslope drainage area, first proposed by Beven and Kirkby [Hydrol. Sci. Bull. 24 (1979) 43]. This new index takes into account the effective rainfall, in addition to topographic factors, in order to achieve a prediction of wetland occurrence for places with different rainy conditions. The two indexes were compared. Six study areas were selected representing a wide range of climate, geology and geomorphology across Europe. The wetland area ranges from I to 30% of the total area for the different catchments, and the annual effective rainfall from 67 to 592 mm. The climato-topographic index seems able to predict the structure and general areal extent of wetlands without any local calibration of the model, except where the permeability of the soil surface is important and very different from the other sites considered. The climato-topographic index gives a classification of wetland occurrence similar to the field data. The exact location of the wetland is often poorly predicted, but this is mostly due to the current poor quality of the Digital Terrain Model. Thus, there is currently a technical limitation to the use of the approach advocated here. (C) 2002 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:51 / 71
页数:21
相关论文
共 63 条
[11]  
BERNARD P, 1994, ZONES HUMIDES RAPPOR, P391
[12]   CATCHMENT GEOMORPHOLOGY AND THE DYNAMICS OF RUNOFF CONTRIBUTING AREAS [J].
BEVEN, K ;
WOOD, EF .
JOURNAL OF HYDROLOGY, 1983, 65 (1-3) :139-158
[13]  
Beven K.J., 1979, HYDROL SCI B, V24, P43, DOI [DOI 10.1080/02626667909491834, 10.1080/02626667909491834]
[14]  
Beven K. J., 1986, SCALE PROBLEMS HYDRO, P107, DOI DOI 10.1007/978-94-009-4678-1_6
[15]   TESTING A PHYSICALLY-BASED FLOOD FORECASTING-MODEL (TOPMODEL) FOR 3 UK CATCHMENTS [J].
BEVEN, KJ ;
KIRKBY, MJ ;
SCHOFIELD, N ;
TAGG, AF .
JOURNAL OF HYDROLOGY, 1984, 69 (1-4) :119-143
[16]   SENSITIVITY TO SPACE AND TIME RESOLUTION OF A HYDROLOGICAL MODEL USING DIGITAL ELEVATION DATA [J].
BRUNEAU, P ;
GASCUELODOUX, C ;
ROBIN, P ;
MEROT, P ;
BEVEN, K .
HYDROLOGICAL PROCESSES, 1995, 9 (01) :69-81
[17]  
Burt T.P., 1997, Buffer Zones: Their Processes and Potential in Water Protection
[18]  
the Proceedings of the International Conference on Buffer Zones, September 1996, P21
[19]   Integrated management of sensitive catchment systems [J].
Burt, TP .
CATENA, 2001, 42 (2-4) :275-290
[20]   TOPOGRAPHIC CONTROLS OF SOIL-MOISTURE DISTRIBUTIONS [J].
BURT, TP ;
BUTCHER, DP .
JOURNAL OF SOIL SCIENCE, 1985, 36 (03) :469-486