scholarly journals Causes of reduced leaf-level photosynthesis during strong El Niño drought in a Central Amazon forest

2018 ◽  
Vol 24 (9) ◽  
pp. 4266-4279 ◽  
Author(s):  
Victor Alexandre Hardt Ferreira dos Santos ◽  
Marciel José Ferreira ◽  
João Victor Figueiredo Cardoso Rodrigues ◽  
Maquelle Neves Garcia ◽  
João Vitor Barbosa Ceron ◽  
...  
2019 ◽  
Vol 10 ◽  
Author(s):  
Bruno O. Gimenez ◽  
Kolby J. Jardine ◽  
Niro Higuchi ◽  
Robinson I. Negrón-Juárez ◽  
Israel de Jesus Sampaio-Filho ◽  
...  

2009 ◽  
Vol 39 (4) ◽  
pp. 1003-1011 ◽  
Author(s):  
Philip Martin Fearnside

Global warming has potentially catastrophic impacts in Amazonia, while at the same time maintenance of the Amazon forest offers one of the most valuable and cost-effective options for mitigating climate change. We know that the El Niño phenomenon, caused by temperature oscillations of surface water in the Pacific, has serious impacts in Amazonia, causing droughts and forest fires (as in 1997-1998). Temperature oscillations in the Atlantic also provoke severe droughts (as in 2005). We also know that Amazonian trees die both from fires and from water stress under hot, dry conditions. In addition, water recycled through the forest provides rainfall that maintains climatic conditions appropriate for tropical forest, especially in the dry season. What we need to know quickly, through intensified research, includes progress in representing El Niño and the Atlantic oscillations in climatic models, representation of biotic feedbacks in models used for decision-making about global warming, and narrowing the range of estimating climate sensitivity to reduce uncertainty about the probability of very severe impacts. Items that need to be negotiated include the definition of "dangerous" climate change, with the corresponding maximum levels of greenhouse gases in the atmosphere. Mitigation of global warming must include maintaining the Amazon forest, which has benefits for combating global warming from two separate roles: cutting the flow the emissions of carbon each year from the rapid pace of deforestation, and avoiding emission of the stock of carbon in the remaining forest that can be released by various ways, including climate change itself. Barriers to rewarding forest maintenance include the need for financial rewards for both of these roles. Other needs are for continued reduction of uncertainty regarding emissions and deforestation processes, as well as agreement on the basis of carbon accounting. As one of the countries most subject to impacts of climate change, Brazil must assume the leadership in fighting global warming.


2000 ◽  
Vol 27 (7) ◽  
pp. 981-984 ◽  
Author(s):  
Gregory P. Asner ◽  
Alan R. Townsend ◽  
Bobby H. Braswell

2021 ◽  
Vol 500 ◽  
pp. 119652
Author(s):  
Paulo Eduardo Barni ◽  
Anelícia Cleide Martins Rego ◽  
Francisco das Chagas Ferreira Silva ◽  
Richard Anderson Silva Lopes ◽  
Haron Abrahim Magalhães Xaud ◽  
...  
Keyword(s):  
El Niño ◽  
El Nino ◽  

2021 ◽  
Vol 502 ◽  
pp. 119712
Author(s):  
Paulo Eduardo Barni ◽  
Anelícia Cleide Martins Rego ◽  
Francisco das Chagas Ferreira Silva ◽  
Richard Anderson Silva Lopes ◽  
Haron Abrahim Magalhães Xaud ◽  
...  
Keyword(s):  
El Niño ◽  
El Nino ◽  

2020 ◽  
Vol 20 (9) ◽  
pp. 5547-5558 ◽  
Author(s):  
Rayonil G. Carneiro ◽  
Gilberto Fisch

Abstract. The Amazon biome contains more than half of the remaining tropical forests of the planet and has a strong impact on aspects of meteorology such as the planetary boundary layer (PBL). In this context, the objective of this study was to conduct observational evaluations of the daily cycle of the height of the PBL during its stable (night) and convective (day) phases from data that were measured and/or estimated using instruments such as a radiosonde, sodar, ceilometer, wind profiler, lidar and microwave radiometer installed in the central Amazon during 2014 (considered a typical year) and 2015 during which an intense El Niño–Southern Oscillation (ENSO) event predominated during the GoAmazon experiment. The results from the four intense observation periods (IOPs) show that during the day and night periods, independent of dry or rainy seasons, the ceilometer is the instrument that best describes the depth of the PBL when compared with in situ radiosonde measurements. Additionally, during the dry season in 2015, the ENSO substantially influenced the growth phase of the PBL, with a 15 % increase in the rate compared to the same period in 2014.


2020 ◽  
Vol 55 (4) ◽  
pp. 1-14
Author(s):  
K. Legal ◽  
P. Plantin
Keyword(s):  
El Niño ◽  

2020 ◽  
Vol 54 (3) ◽  
pp. 1-15
Author(s):  
K. Legal ◽  
P. Plantin
Keyword(s):  
El Niño ◽  

Author(s):  
C. Thévenin-Lemoine ◽  
F. Accadbled ◽  
J. Sales de Gauzy
Keyword(s):  
El Niño ◽  

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