Guianan forest dynamics: geomorphographic control and tropical forest change across diverging landscapes.

Author(s):  
D. S. Hammond
2009 ◽  
Vol 106 (44) ◽  
pp. 18621-18626 ◽  
Author(s):  
W. J. Kress ◽  
D. L. Erickson ◽  
F. A. Jones ◽  
N. G. Swenson ◽  
R. Perez ◽  
...  

2020 ◽  
Vol 9 (10) ◽  
pp. 580 ◽  
Author(s):  
Maria Antonia Brovelli ◽  
Yaru Sun ◽  
Vasil Yordanov

Deforestation causes diverse and profound consequences for the environment and species. Direct or indirect effects can be related to climate change, biodiversity loss, soil erosion, floods, landslides, etc. As such a significant process, timely and continuous monitoring of forest dynamics is important, to constantly follow existing policies and develop new mitigation measures. The present work had the aim of mapping and monitoring the forest change from 2000 to 2019 and of simulating the future forest development of a rainforest region located in the Pará state, Brazil. The land cover dynamics were mapped at five-year intervals based on a supervised classification model deployed on the cloud processing platform Google Earth Engine. Besides the benefits of reduced computational time, the service is coupled with a vast data catalogue providing useful access to global products, such as multispectral images of the missions Landsat five, seven, eight and Sentinel-2. The validation procedures were done through photointerpretation of high-resolution panchromatic images obtained from CBERS (China–Brazil Earth Resources Satellite). The more than satisfactory results allowed an estimation of peak deforestation rates for the period 2000–2006; for the period 2006–2015, a significant decrease and stabilization, followed by a slight increase till 2019. Based on the derived trends a forest dynamics was simulated for the period 2019–2028, estimating a decrease in the deforestation rate. These results demonstrate that such a fusion of satellite observations, machine learning, and cloud processing, benefits the analysis of the forest dynamics and can provide useful information for the development of forest policies.


Vegetatio ◽  
1995 ◽  
Vol 121 (1-2) ◽  
pp. 41-52 ◽  
Author(s):  
Soedarsono Riswan ◽  
Lies Hartanti

2008 ◽  
Vol 148 (5) ◽  
pp. 748-760 ◽  
Author(s):  
A.R. Huete ◽  
N. Restrepo-Coupe ◽  
P. Ratana ◽  
K. Didan ◽  
S.R. Saleska ◽  
...  

2004 ◽  
Vol 20 (01) ◽  
pp. 51-72 ◽  
Author(s):  
Richard Condit ◽  
Salomon Aguilar ◽  
Andres Hernandez ◽  
Rolando Perez ◽  
Suzanne Lao ◽  
...  

2005 ◽  
Vol 62 (8) ◽  
pp. 785-796 ◽  
Author(s):  
Sylvie Gourlet-Fleury ◽  
Lilian Blanc ◽  
Nicolas Picard ◽  
Plinio Sist ◽  
Jan Dick ◽  
...  

2018 ◽  
Vol 34 (3) ◽  
pp. 157-175 ◽  
Author(s):  
John B. Vincent ◽  
Benjamin L. Turner ◽  
Clant Alok ◽  
Vojtech Novotny ◽  
George D. Weiblen ◽  
...  

Abstract:Long-term forest dynamics plots in the tropics tend to be situated on stable terrain. This study investigated forest dynamics on the north coast of New Guinea where active subduction zones are uplifting lowland basins and exposing relatively young sediments to rapid weathering. We examined forest dynamics in relation to disturbance history, topography and soil nutrients based on partial re-census of the 50-ha Wanang Forest Dynamics Plot in Papua New Guinea. The plot is relatively high in cations and phosphorus but low in nitrogen. Soil nutrients and topography accounted for 29% of variation in species composition but only 4% of variation in basal area. There were few areas of high biomass and most of the forest was comprised of small-diameter stems. Approximately 18% of the forest was less than 30 y old and the annual tree mortality rate of nearly 4% was higher than in other tropical forests in South-East Asia and the neotropics. These results support the reputation of New Guinea's forests as highly dynamic, with frequent natural disturbance. Empirical documentation of this hypothesis expands our understanding of tropical forest dynamics and suggests that geomorphology might be incorporated in models of global carbon storage especially in regions of unstable terrain.


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