| Grant number: | 13/50531-2 |
| Support Opportunities: | Research Program on Global Climate Change - Regular Grants |
| Start date: | January 01, 2014 |
| End date: | December 31, 2017 |
| Field of knowledge: | Physical Sciences and Mathematics - Geosciences |
| Agreement: | GOAmazon Collaborative Research |
| Principal Investigator: | Laura de Simone Borma |
| Grantee: | Laura de Simone Borma |
| Principal researcher abroad: | Jung-Eun Lee |
| Institution abroad: | Brown University , United States |
| Host Institution: | Instituto Nacional de Pesquisas Espaciais (INPE). São José dos Campos , SP, Brazil |
| City of the host institution: | São José dos Campos |
Abstract
The Amazon currently plays a criticaI role in the terrestrial climate system, in terms of, e.g., regulating carbon stocks and supporting high biodiversity and endemism. Over the last decade, Amazonian forests have begun experiencing more frequent dry periods, including two extreme drought episodes in 2005 and 2010. However, the future of the Amazon as projected by current generation climate or earth system models is highly uncertain: how global warming and other aspects of anthropogenic change such as deforestation and degradation will ultimately impact this system is far from clear. A dominant source of uncertainty regarding Amazonian climate and its future evolution is the role of land-vegetation-atmosphere coupling, especially interactions of and feedbacks between vegetation and precipitating deep convection occurring during the late dry season/early wet season when land-vegetation-atmosphere coupling has been shown to be stronger. Quantitative understanding of this coupling is criticaI since forest productivity is sensitive to the duration and intensity of the dry season. Thus, our principal objective is to address how vegetation influences climate variability and precipitation over Amazonian rainforests, with an emphasis on plant physiological controls on deep convection triggering along a geographical water stress gradient. To support this objective, our proposed research comprises three interrelated activities: (i) in situ measurements of plant physiological water stress with a focus on fluorescence and its control on surface energy and water budgets as observed at existing flux tower sites; (ii) diagnostic analysis of plant physiological parameters and processes, observed surface turbulent fluxes, boundary layer properties, and cloud cover and precipitation along a moisture gradient; and (iii) process-based model studies of the pathways through which the surface energy partitioning (Bowen ratio) and transpiration, as modified by water stress, influence convection both locally and non-locally. These activities cut across programmatic objectives expressed by ali 3 of the DOE BER research programs supporting GOAmazon. Moreover, the synthesis of new in-situ fluorescence data combined with existing or planned ground and satellite observations and process studies with models of varying levels of complexity is ultimately expected to inform the development and implementation of representations of coupled land-vegetation-atmosphere processes in state-of-the-art climate models (e.g., the NCAR CLM-CAM). (AU)
| Articles published in Agência FAPESP Newsletter about the research grant: |
| More itemsLess items |
| TITULO |
| Articles published in other media outlets ( ): |
| More itemsLess items |
| VEICULO: TITULO (DATA) |
| VEICULO: TITULO (DATA) |