Although they make up only 1 % of all tropical forest areas, the thickness of this carbon - rich layer means mangroves hold as much as a quarter of the carbon of
tropical peat lands.
Muddy mangrove swamps hold onto as much 25 % of the carbon stored in similarly threatened
tropical peat lands - despite covering a much smaller area.
«These results show that biofuels causing any significant expansion of palm on
tropical peat will actually increase emissions relative to petroleum fuels.
so many climatic tipping points will have been passed that global warming will become self perpetuating release of methane from permafrost and under Arctic Ocean, release of carbon from
tropical peat, loss of sea and forests as carbon sink etc..
These warming regimes will also drive rapid emissions from
tropical peat, through tropical rainforest drying and through heat stresses on boreal forests.
Tropical peat fires release phenomenal amounts of greenhouse gases.
These Arctic and high - latitude peat fires might not immediately affect as many people as
tropical peat fires, because for the most part the fires aren't in agricultural hot spots or urban centers.
This report provides an independent review of available scientific information and published literature on impacts of the use of
tropical peat for oil palm cultivation in Southeast Asia.
Not exact matches
But changes in land use — draining the water to plant acres of crops that demand drier soil, a common practice in
tropical regions, or building a road through an area — can dry out the
peat.
A study published in August 2017 in Global Change Biology used data on where water accumulates and how it flows across the landscape to predict where
peat might be hiding in
tropical regions.
Indonesia's sprawling
tropical forests and
peat soils act as a massive carbon storage sink but have been heavily deforested and degraded in recent years, primarily by palm oil companies and the pulp - paper giants Asian Pulp and Paper and Asia Pacific Resources International Ltd..
If humans continue to convert the gigantic biomass of
tropical forests and
peat bogs into carbon in the sky, it may not matter if you install solar panels on your home, or stop flying.
The fossils were formed in a swampy
peat bog of a
tropical to subtropical environment where plant tissues were preserved through rapid silicate diagenesis.
These are the truly unnatural fires as
tropical wet forests (and
peat fires too) are not supposed to burn but do so because of unsustainable land - uses.
In contrast, RED would be more effective in terms of its conservation impact if payments were extended to all remaining carbon - rich
tropical forests, including lowland
peat swamp forests, the preferred habitat for dense populations of orangutans, and if the construction of new roads was halted.
Woody plantations crops like oil palm and coconut rate much better, although their advantages are reduced when they are grown in place of carbon - rich
tropical rainforests and
peat lands.
And they found that the highest post-thaw emissions of nitrous oxide came from the bare
peat soils: these emissions were fivefold those from still - frozen soils and matched the kind of outgassing observed in
tropical soils, which are the world's largest natural land - based nitrous oxide source.
The report describes the Leuser Ecosystem as «a rich and verdant expanse of intact
tropical lowland rainforests, cloud draped mountains and steamy
peat swamps.
But
peat is also a massive store of carbon, described as Europe's equivalent of the
tropical rainforest.
Tropical deforestation releases more than 1.5 billion metric tons of carbon into the atmosphere every year, though in some years, like the 1997 - 1998 el Nino year when fires released some 2 billion tons of carbon from
peat swamps alone in Indonesia, emissions are more than twice that.
Borneo's
peat lands going up in smoke Fire in the
Peat Lands Borneo's
peat lands going up in smoke Tina Butler, mongabay.com April 21, 2005 The
tropical rainforests of Kalimantan...
Our recent story on carbon emissions from
tropical forests shows possibly the most prominent example, but Arctic and many other
peat bogs must also be regarded as strategic.
Coal deposits are compressed
peat swamps that began as dry - land
tropical forests.
Indonesian forests are home to roughly 60 percent of the world's
tropical peatlands, where decayed vegetation or organic matter has accumulated in the soil layers and created
peat deposits that can be up to 10 meters deep.
Tropical wetlands, including palm swamps and mangroves, are important carbon sinks, but as much as 80 percent of that carbon is stored in a submerged layer of
peat.
In order of seniority, the seven feedbacks that seem outstanding are: Water vapour — rising by ~ 7 % per 1.0 C of warming; Albedo loss — due mostly to cryosphere decline; Microbial
peat - bog decay — due to rising CO2 affecting ecological dynamics; Desiccation of
tropical and temperate soils — due to SAT rise and droughts; Permafrost melt — due to SAT rise plus loss of snow cover, etc; Forest combustion — due to SAT rise, droughts, pest responses, etc; Methyl clathrates [aka methane hydrates] now threatened by rising sea - temperatures, increased water column mixing, etc..
The importance of preserving
tropical wetlands — mangrove and
peat forests — is ever clearer.
Because creating the plantations often means burning the
tropical forest and draining the underlying
peat soils, there's an initial large release of stored carbon.
65 % of the world's
tropical peatlands are located in Indonesia, and when plantations are established on
peat, emissions are even worse.