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The role of El Niño in modulating the effects of deforestation in the Maritime Continent

Bibliographic Data

ID15550378
AuthorsTing‐Hui Lee (0009-0004-4073-2596, National Taiwan University), Ting-Hui Lee, Min‐Hui Lo (0000-0002-8653-143X, National Taiwan University, corresponding author)
Year2021
Volume16
Issue5
Pages054056-054056
Publication date2021-02-22
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/abe88e
OpenAlexW3132982652
LanguageEN
References cited28

The deforestation rate in the Maritime Continent (MC) has been accelerating during the past several decades. Understanding the changes in local hydro-climatological cycles as deforestation takes place is essential because the MC is suffering from frequent and extreme droughts and fires, which often occur during the dry season and are more severe during El Niños. Therefore, this study explores how deforestation affects the hydrological cycle and precipitation in the MC during El Niños, focusing on the boreal autumn season and using the coupled atmosphere–land model simulations. It is found that the precipitation over the MC increases in the deforestation experiments, and the precipitation responses can be magnified during El Niño events. A strong subsidence anomaly associated with El Niño does not prevent enhanced convection associated with local deforestation. Instead, the subsidence reduces the cloud cover in the MC region during El Niño, which increases the incoming solar radiation and increases surface temperatures. Thus, a warmer environment induced by El Niño modulates the biogeophysical feedbacks associated with deforestation that also play a critical role in more substantial land surface warming. A warmer land surface induces a more unstable atmospheric environment associated with a tendency toward enhanced local convection and lateral moisture convergence. This study highlights how the different mean climate states may modulate the impact of local land-use changes on hydroclimatological cycles in the MC, and sheds light on the state of our knowledge of interactions between the local land surface and remote large-scale atmospheric circulations

Atmosphere (unit · Atmospheric sciences · Climate change · Climate model · Climatology · Cloud computing · Cloud cover · Convection · Deforestation (computer science · Geography · Geomorphology · Meteorology · Precipitation · Structural basin · Subsidence · Water cycle · Climate variability and models · Environmental Science · Geology and Paleoclimatology Research · Oceanographic and Atmospheric Processes · Ecology · Geology · Oceanography

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Highly citedNo

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