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1.
Proc Natl Acad Sci U S A ; 104(12): 4820-3, 2007 Mar 20.
Artigo em Inglês | MEDLINE | ID: mdl-17360360

RESUMO

Despite early speculation to the contrary, all tropical forests studied to date display seasonal variations in the presence of new leaves, flowers, and fruits. Past studies were focused on the timing of phenological events and their cues but not on the accompanying changes in leaf area that regulate vegetation-atmosphere exchanges of energy, momentum, and mass. Here we report, from analysis of 5 years of recent satellite data, seasonal swings in green leaf area of approximately 25% in a majority of the Amazon rainforests. This seasonal cycle is timed to the seasonality of solar radiation in a manner that is suggestive of anticipatory and opportunistic patterns of net leaf flushing during the early to mid part of the light-rich dry season and net leaf abscission during the cloudy wet season. These seasonal swings in leaf area may be critical to initiation of the transition from dry to wet season, seasonal carbon balance between photosynthetic gains and respiratory losses, and litterfall nutrient cycling in moist tropical forests.


Assuntos
Folhas de Planta/anatomia & histologia , Folhas de Planta/crescimento & desenvolvimento , Estações do Ano , Árvores/anatomia & histologia , Árvores/crescimento & desenvolvimento , Brasil , Geografia , Tamanho do Órgão , Folhas de Planta/efeitos da radiação , Chuva , Comunicações Via Satélite/instrumentação , Luz Solar , Fatores de Tempo , Árvores/efeitos da radiação
2.
J Chem Phys ; 123(23): 234502, 2005 Dec 15.
Artigo em Inglês | MEDLINE | ID: mdl-16392926

RESUMO

The particle-transfer molecular-dynamics technique is adopted to construct the Lennard-Jones fluid gas-liquid phase diagram. Detailed study of the dependence of the simulation results on the system size and the cutoff distance is performed to test the validity of the simulation technique. Both the traditional cutoff plus long-range correction (CPC) and Ewald summation methods are used in the simulations to calculate the interactions. In the intermediate range of temperatures, the results with the Ewald summation method are almost the same as those with the CPC method. However, in the range close to the critical point, the results with the CPC method deviate from those with the Ewald summation. Compared with the results obtained via the Ewald summation in a smaller system, simply increasing the system size in the CPC scheme may not give better results.

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