{"id":1040,"date":"2026-07-10T11:54:03","date_gmt":"2026-07-10T11:54:03","guid":{"rendered":"https:\/\/redzine.co.uk\/index.php\/2026\/07\/10\/tropical-forests-can-switch-from-carbon-sinks-to-carbon-sources-during-el-nino\/"},"modified":"2026-07-10T11:54:03","modified_gmt":"2026-07-10T11:54:03","slug":"tropical-forests-can-switch-from-carbon-sinks-to-carbon-sources-during-el-nino","status":"publish","type":"post","link":"https:\/\/redzine.co.uk\/index.php\/2026\/07\/10\/tropical-forests-can-switch-from-carbon-sinks-to-carbon-sources-during-el-nino\/","title":{"rendered":"Tropical forests can switch from carbon sinks to carbon sources during El Ni\u00f1o"},"content":{"rendered":"
South American tropical forests risk turning from carbon sinks to carbon sources during extreme climate events like El Ni\u00f1o.<\/span> Teo Tarras \/ Shutterstock<\/a><\/span><\/figcaption><\/figure>\n

Tropical forests draw down and store large quantities of CO\u2082 from the atmosphere. The Amazon rainforest in South America, for example, stores approximately 123 billion tonnes<\/a> of carbon \u2013 more than is stored in any other terrestrial ecosystem in the world. But these forests are facing a critical challenge. <\/p>\n

Research from 2023<\/a>, which was carried out by me and more than 100 colleagues, found that tropical forests in South America are vulnerable to climate extremes. We determined that during an El Ni\u00f1o event, the warm phase of a natural fluctuation in the Earth\u2019s climate system, South American tropical forests may fail to act as a carbon sink.<\/p>\n

This finding becomes even more alarming when we consider<\/a> the increasing frequency and intensity of El Ni\u00f1o events. There have been twice as many \u201cvery strong\u201d El Ni\u00f1os in the last 60 years as there were in the 60 years before that. And the US National Oceanic and Atmospheric Administration has recently confirmed that<\/a> such an El Ni\u00f1o is currently underway.<\/p>\n

Tropical forests absorb CO\u2082 through the process of photosynthesis and convert it into biomass. However, the balance between photosynthesis and respiration is delicate and depends on two factors: temperature and water availability. <\/p>\n

In hotter and drier conditions, plants close the pores of their leaves to avoid water loss. But closing them effectively cuts off a plant\u2019s fuel supply because it is through these pores they absorb CO\u2082. This starves plants of the carbon needed for photosynthesis and to grow. <\/p>\n

During El Ni\u00f1o years, which are characterised by high temperature anomalies<\/a>, prolonged climate stress leads to reduced forest growth and increased tree mortality. The effects of this are felt for decades as carbon is released back into the atmosphere when the dead trees decompose.<\/p>\n

Our findings revealed that during the 2015-2016 El Ni\u00f1o, when temperatures on land were at least a degree higher on average than usual conditions, some of South America\u2019s tropical forests effectively stopped absorbing carbon. This raises concerns about the possible impact of the current El Ni\u00f1o<\/a> on the Amazon and global climate.<\/p>\n

\n \"A<\/a>
\n The Amazon rainforest covers much of north-western Brazil and extends into Colombia, Peru and other South American countries.<\/span>
\n Rainer Lesniewski \/ Shutterstock<\/a><\/span>
\n <\/figcaption><\/figure>\n

In our research, we measured over half a million trees across six South American countries over a period of more than 30 years, using tape measures to track their growth. These trees belonged to over 4,000 different species. We used this data to calculate precise estimates of the amount of carbon stored as a forest\u2019s aboveground biomass.<\/p>\n

We found that the vulnerability of these forests to El Ni\u00f1o conditions was closely linked to their baseline climate. While we tend to assume that rainforests are all hot, wet and biodiverse ecosystems, seasonal drought is a reality for many tropical forests. Conditions in regions at the edge of the Amazon rainforest, for example, tend to be particularly hot and dry.<\/p>\n

Our findings revealed that drier forests at the edge of the Amazon, where trees regularly endure periods of limited water availability, were especially susceptible to extreme El Ni\u00f1o conditions. On average, a 0.5\u00b0C increase in temperature caused these forests to lose 0.5% of their aboveground carbon.<\/p>\n

Larger trees suffered the most<\/a>. While tree mortality rates increased from 1.8% to 3% per year during the El Ni\u00f1o in South American tropical forests as a whole, mortality rates effectively doubled for medium (classified as over 20cm in diameter) and large trees.<\/p>\n

The fact that larger trees with less dense wood died at much higher rates compared to small trees and those with high wood density points strongly to hydraulic failure, when intense atmospheric moisture demand snaps the tension in the tree\u2019s internal water column rather than slow carbon starvation.<\/p>\n

These results suggest that adaption to seasonal drought may not be sufficient to protect tropical forests from extreme events. Climate extremes are possibly already pushing forests at the edges of the Amazon beyond their capacity to adapt, causing catastrophic carbon losses.<\/p>\n

A looming threat<\/h2>\n

Scientists have warned that 2026 may again be the warmest year on record. Heightening the alarm further is the severity of the current El Ni\u00f1o. Never before has an an El Ni\u00f1o begun when oceans are already so warm and air temperatures so high.<\/p>\n

On top of this is the fact that, over the past three decades, the edges of the Amazon have experienced some of the highest temperatures and most rapid warming<\/a> the tropics have ever seen. The structural integrity of a forest is compromised when a major climate anomaly occurs before it has recovered from recent, multi-year stress. <\/p>\n

These compounding factors mean that we risk witnessing tree and carbon losses on scales not yet seen.<\/p>\n

\n \"A
\n During the 2015-2016 El Ni\u00f1o, some of South America\u2019s tropical forests effectively stopped absorbing carbon.<\/span>
\n Cavan-Images \/ Shutterstock<\/a><\/span>
\n <\/figcaption><\/figure>\n

Tropical forests are invaluable assets in the fight against climate change. But South American tropical forests, a once-reliable carbon sink, are vulnerable to intensifying heat and drought. There is a risk these essential ecological allies stop acting as a carbon sink<\/a> as extreme climate conditions become the norm.<\/p>\n

Preserving tropical forests is thus essential. Their ability to continue acting as carbon sinks hinges on efforts to protect them and a collective commitment to limit global temperature rise. The Amazon\u2019s future depends on this, and so does ours.<\/p>\n

\"The<\/p>\n

Amy Bennett receives funding from the European Space Agency, the UK Natural Environment Research Council and the Royal Society.
\n<\/span><\/em><\/p>\n","protected":false},"excerpt":{"rendered":"

South American tropical forests risk turning from carbon sinks to carbon sources during extreme climate events like El Ni\u00f1o. Teo Tarras \/ Shutterstock Tropical forests draw down and store large quantities of CO\u2082 from the atmosphere. The Amazon rainforest in South America, for example, stores approximately 123 billion tonnes of carbon \u2013 more than is […]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-1040","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/posts\/1040","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/comments?post=1040"}],"version-history":[{"count":0,"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/posts\/1040\/revisions"}],"wp:attachment":[{"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/media?parent=1040"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/categories?post=1040"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/redzine.co.uk\/index.php\/wp-json\/wp\/v2\/tags?post=1040"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}