scholarly journals Wood plenty, grass good, water none: Vegetation changes in Arizona's upper Verde River watershed from 1850 to 1997

Author(s):  
Harley G. Shaw
1970 ◽  
Vol 48 (11) ◽  
pp. 1957-1975 ◽  
Author(s):  
Alastair Morrison

Six pollen zones can be distinguished in interior Labrador. The earlier zones represent the primary succession of vegetation from bare ground to boreal woodland or forest, which occupied about 500 years between 5700 and 5200 B.P. There have been only minor fluctuations in the nature of the vegetation since 5200 B.P. Radiocarbon dates show that the zones are contemporaneous over that part of the Lake Plateau within the Churchill River watershed, but similar vegetation changes occurred 1000 years earlier in the Kaniapiskau basin, further north, in New Quebec. These two areas must have been freed of a cover of glacier ice or lake waters immediately before 5700 B.P. and 6700 B.P. respectively.


Author(s):  
Nicholas V. Paretti ◽  
Anne M. D. Brasher ◽  
Susanna L. Pearlstein ◽  
Dena M. Skow ◽  
Bruce W. Gungle ◽  
...  

2019 ◽  
Vol 109 ◽  
pp. 101999
Author(s):  
Xiaobing Zhao ◽  
Ding Du ◽  
Jun Xiong ◽  
Abraham Springer ◽  
Sharon R. Masek Lopez ◽  
...  

Author(s):  
Lívia Alves Alvarenga ◽  
Vinícius Siqueira Oliveira Carvalho ◽  
Vinícius Augusto de Oliveira ◽  
Carlos Rogério de Mello ◽  
Alberto Colombo ◽  
...  

Successful streamflow forecasts depend on an adequate performance evaluation of the hydrological model. In this study, the hydrological responses were compared using two hydrological models, physic-based and semi-distributed, Soil and Water Assessment Tool (SWAT) and Variable Infiltration Capacity (VIC), using input data from the Verde River Watershed, located in the Minas Gerais state in southern Brazil. This is a study of one of the most important headwater watershed regions of Brazil (Mantiqueira Range). Both models were suitable for streamflow simulation, with values of R2 (determination coefficient) and NSE (Nash-Sutcliffe) higher than 0.8, NSELog higher than 0.35 (Nash–Sutcliffe Efficiency of the logarithmic values of discharge) and PBIAS (percentage deviation) less than 25%. The integration of SWAT and VIC models can be useful in different water-resource assessment studies. Therefore, based upon this study further investigations should be conducted using various hydrological models and climate, land-use and land-cover changes scenarios in the region.


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