We found that
soil warming results in a four - phase pattern of soil organic matter decay and carbon dioxide fluxes to the atmosphere, with phases of substantial soil carbon loss alternating with phases of no detectable loss.
Not exact matches
When the researchers simulated a second effect of climate change in addition to
warming, namely drought, the
results were even the opposite as expected: The
soil animals ate less, and also the microorganisms living in the
soil showed a decline in respiration — an indication that they also consumed less food.
Our
results indicate that it may not be the
soil animals, on the contrary: Their role may actually be the opposite of what we expected, at least when
warming and drought occur together.»
The
results suggest that
soil respiration and organic carbon decomposition in the tundra, especially in grassy areas, will increase with
warming temperatures and rising
soil moisture,
resulting in increased carbon dioxide emissions to the atmosphere.
«This study addresses this knowledge gap by showing that
warming increased plant biomass, but also redistributes carbon into the
soil resulting in no change in
soil [carbon] stocks.»
Estimates are that microbial respiration will speed up as the
soil warms,
resulting in a net flux of CO2 to the atmosphere.
The only argument I've seen along those lines is the one that claims that the vast majority of the CO2 humans are emitting is sequestered in
soils, oceans, etc, or used by plants, but that «naturally»
warmer temps
result in the release of sequestered CO2.
Warmer temperatures at high latitudes are already
resulting more frequent Arctic fires, and unprecedented permafrost thaw is leaving large
soil carbon pools exposed to smoldering fires for the fist time since ancient times.
Estimates are that microbial respiration will speed up as the
soil warms,
resulting in a net flux of CO2 to the atmosphere.
The
results indicate that next to SWEmax (which strongly controls the annual maximum of
soil moisture), the snowmelt rate, the ENSO and PDO indices, and rate of
warming subsequent to the date of SWEmax are the most influential predictors of APF magnitude in the FRB and its subbasins.
Warming results in more carbon dioxide release from
soil and peat moss — it is some 20 % of the fossil fuel emissions.
As a
result, the peaks in California's snow melt and surface runoff are likely to be more pronounced and to occur earlier in the calendar year, increasing the duration of the
warm - season low - runoff period and potentially reducing surface
soil moisture.
9 Effects of Global
Warming Rising Sea Levels Rising Sea Levels
Result in
Soil Erosion Flooding Loss of Homes Loss of Life
E.g., research assumes greenhouse gas emissions cause
warming without explicitly stating humans are the cause»... carbon sequestration in
soil is important for mitigating global climate change» (4a) No position Does not address or mention the cause of global
warming (4b) Uncertain Expresses position that human's role on recent global
warming is uncertain / undefined «While the extent of human - induced global
warming is inconclusive...» (5) Implicit rejection Implies humans have had a minimal impact on global
warming without saying so explicitly E.g., proposing a natural mechanism is the main cause of global
warming»... anywhere from a major portion to all of the
warming of the 20th century could plausibly
result from natural causes according to these
results» (6) Explicit rejection without quantification Explicitly minimizes or rejects that humans are causing global
warming»... the global temperature record provides little support for the catastrophic view of the greenhouse effect» (7) Explicit rejection with quantification Explicitly states that humans are causing less than half of global
warming «The human contribution to the CO2 content in the atmosphere and the increase in temperature is negligible in comparison with other sources of carbon dioxide emission»»
From the Southwest to the Great Lakes, temperatures have been so high and rainfall so low that the drying effect of
warmer air temperatures far exceeded what little precipitation there's been,
resulting in moisture being drawn out of
soils.
Warming has
resulted in a complex pattern of net carbon loss from the
soil.
Although the melting of underlying permafrost will release huge amounts of the greenhouse gases blamed for fueling global
warming, researchers who sampled three sites in boreal Alberta, Saskatchewan and Manitoba have discovered that the
warmer, softer, wetter
soil that
results also promotes the growth of new mosses that capture and store about as much carbon from the atmosphere as the thawed ground releases.
This
result suggests that the reduced precipitation has caused drier
soils, which in turn have enhanced the
warming owing to reduced cooling by evaporation.
When done so, proxy records and climate models indicate that the response to past global
warming was profound, with evidence for global reorganisation of the hydrological cycle and profound local increases and decreases in rainfall; combined with elevated temperatures and terrestrial vegetation change, this appears to often
result in
warming - enhanced
soil organic matter oxidation, chemical weathering and nutrient cycling.
While deforestation has been the focus of most research into forests» effects on climate change, with a recent study suggesting tropical forests are turning into carbon sources rather than carbon stores as a
result, the impact of
warming soils has remained much of a mystery.