Large Seasonal Swings in Leaf Area of Amazon Rainforests

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...

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Published inProceedings of the National Academy of Sciences - PNAS Vol. 104; no. 12; pp. 4820 - 4823
Main Authors Myneni, Ranga B., Yang, Wenze, Nemani, Ramakrishna R., Huete, Alfredo R., Dickinson, Robert E., Knyazikhin, Yuri, Didan, Kamel, Fu, Rong, Juárez, Robinson I. Negrón, Saatchi, Sasan S., Hashimoto, Hirofumi, Ichii, Kazuhito, Shabanov, Nikolay V., Tan, Bin, Ratana, Piyachat, Privette, Jeffrey L., Morisette, Jeffrey T., Vermote, Eric F., Roy, David P., Wolfe, Robert E., Friedl, Mark A., Running, Steven W., Votava, Petr, El-Saleous, Nazmi, Devadiga, Sadashiva, Su, Yin, Salomonson, Vincent V.
Format Journal Article
LanguageEnglish
Published United States National Academy of Sciences 20.03.2007
National Acad Sciences
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Summary: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 ≈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.
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Author contributions: R.B.M. and A.R.H. designed research; Y.K., R.I.N.J., H.H., K.I., N.V.S., B.T., P.R., and M.A.F. performed research; R.R.N., R.F., R.I.N.J., S.S.S., H.H., K.I., J.L.P., J.T.M., E.F.V., D.P.R., R.E.W., M.A.F., S.W.R., P.V., N.E.-S., S.D., and V.V.S. contributed new reagents/analytic tools; W.Y., K.D., and Y.S. analyzed data; and R.B.M., A.R.H., R.E.D., R.F., J.L.P., J.T.M., E.F.V., D.P.R., and S.W.R. wrote the paper.
lPresent address: Remote Sensing and Applications Division, National Oceanic and Atmospheric Administration, National Climatic Data Center, 151 Patton Avenue, Asheville, NC 28801.
bPresent address: Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, 2455 Hayward Street, Ann Arbor, MI 48109.
Contributed by Robert E. Dickinson, December 22, 2006
jPresent address: Earth Resources Technology, Inc., 10810 Guilford Road, Suite 105, Annapolis Junction, MD 20701.
ISSN:0027-8424
1091-6490
DOI:10.1073/pnas.0611338104