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Feedbacks between vegetation and rainfall in the Amazon basin
Auteur(s)
Maison d'édition
Berlin : Mathematisch-Naturwissenschaftliche Fakultät
Date de parution
2016
Nombre de page
142
Résumé
The distribution of rainfall and vegetation are closely interconnected in the Amazon basin. Rainforests maintain atmospheric humidity by evapotranspiration, which eventually contributes to regional rainfall but also to rainfall over subtropical South America. A comprehensive understanding of the complex interactions between the terrestrial and atmospheric components of the hydrological cycle that occur as moist air is transported by winds over land is missing. The rst aim of this thesis is to ll this gap in knowledge by means of complex network analysis of water uxes from the sources to the sinks of rainfall on the continent. Using this novel approach, the concept of cascading moisture recycling" is introduced, de ned as moisture recycling on the continent involving \reevaporation cycles" (evaporation of precipitating moisture in the same location) along the way. A methodological framework is developed to quantify the importance of cascading moisture recycling and to identify key regions where re-evaporation cycles are taking place. Applied to several combinations of observation-based gridded climate data for South America, it reveals, for instance, that the southern part of the Amazon basin is not only a direct source of rainfall for the La Plata basin (as previously thought) but also an intermediary region that re-distributes moisture evaporating from the entire Amazon basin towards the subtropics. This new concept lays the foundation for evaluating the vulnerability of the Amazon forest to environmental perturbations, which is the second aim of this thesis. Land-use and rainfall variability are expected to be intensi ed at the end of the twenty- rst century and may push the south-eastern part of the Amazon forest towards a grass-dominated ecosystem. Such a forest loss would reduce local dryseason
evapotranspiration and the resulting moisture supply for down-wind rainfall. Inturn, this might erode the resilience of the remaining forest and lead to further forest losses. Using a complex network approach, the concepts of forest resilience and cascading moisture recycling are combined in a data-driven modeling framework. Key regions are identi ed where deforestation would greatly destabilize the remaining forest, as well as tipping points in dry-season intensi cation for large-scale self-ampli ed Amazon forest loss. The ndings highlight the need to maintain the diversity and connectivity of forest patches in order to sustain the ecological integrity of the largest remaining tropical forest on Earth.
evapotranspiration and the resulting moisture supply for down-wind rainfall. Inturn, this might erode the resilience of the remaining forest and lead to further forest losses. Using a complex network approach, the concepts of forest resilience and cascading moisture recycling are combined in a data-driven modeling framework. Key regions are identi ed where deforestation would greatly destabilize the remaining forest, as well as tipping points in dry-season intensi cation for large-scale self-ampli ed Amazon forest loss. The ndings highlight the need to maintain the diversity and connectivity of forest patches in order to sustain the ecological integrity of the largest remaining tropical forest on Earth.
Notes
Humboldt-Universität zu Berlin, Mathematisch-Naturwissenschaftliche Fakultät 2016
Identifiants
Type de publication
doctoral thesis
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