Climate change and the eco-hydrology of fire: will area burned
increase in a warming western US?
Not exact matches
Overall, aquatic ecosystems
in western North America are predicted to experience increasingly earlier snowmelt
in the spring, reduced late spring and summer flows,
warmer and drier summers, and
increased water temperatures — all of which spell
increased hybridization between these species.
While the pattern for Central and
Western Europe was one of a consistent
increase in flood risk, the study also found that flood risk may actually decrease with
warmer temperatures
in some countries
in Eastern Europe, but those results also show a high degree of uncertainty.
A study assesses flood impacts for three scenarios — of 1.5 °C, 2 °C and 3 °C
warming — and finds that most of Central and
Western Europe will experience substantial
increase in flood risk at all
warming levels, and the higher the
warming, the higher the risk.
Three of the four
warmest years since 1900 have been years with El Niño — the phenomenon
in which
warm water from the
western side of the equatorial Pacific sloshes east,
increasing global temperatures.
As the climate has
warmed,
western forests have suffered both an
increase in stress and
increased beetle overwintering survival, which gives advantage to the bark beetles.
This shift from cool to
warm in the North Atlantic has already had an impact; this past year at least 89,000 individual fires burned 9.5 million acres
in the
western U.S. Worse yet, forest management practices that have
increased the number of trees
in western woods — as well as relatively wet preceding decades — have put
in place an abundance of fuel for future fires.
«There are characteristic patterns of
increase and decrease, for example,
in response to an El Nino event,» which is a cyclical climate event marked by
warming waters
in the
western Pacific Ocean that has global impacts, Zwiers says.
«It confirms that the during the Medieval
Warm Period between 1080 and 1430 the oscillation index was
in an unusually prolonged positive phase, which brings
increased rain to Scotland and drier conditions
in the
western Mediterranean,» says Baker, of the UNSW Connected Waters Initiative Research Centre.
Abstract — James L. Crowley — 12 November 2010 Effects of Rapid Global
Warming at the Paleocene - Eocene Boundary on Neotropical Vegetation Temperatures
in tropical regions are estimated to have
increased by 3 ° to 5 °C, compared with Late Paleocene values, during the Paleocene - Eocene Thermal Maximum (PETM, 56.3 million years ago)......... eastern Colombia and
western Venezuela.
MHW intensity between 1982 — 1998 and 2000 — 2016
increased in over 65 % of the global ocean, most notably
in all five
western boundary current regions, where the mean
warming has been considerably faster than the global average39, and most mid-latitude ocean basins (Fig. 1e).
You can read a more recent discussion of the role the bark beetle and climate change are playing
in burning down and reshaping the West
in this National Wildlife Federation report, «
Increased Risk of CatastrophicWildfires: Global
Warming's Wake - Up Call for the
Western United States.»
Hence, the projected regional
warming and consequent
increase in wildfire activity
in the
western United States is likely to magnify the threats to human communities and ecosystems, and substantially
increase the management challenges
in restoring forests and reducing greenhouse gas emissions.
In Relationships between Water Vapor Path and Precipitation over the Tropical Oceans, Bretherton et al showed that although the Western Pacific warmer surface waters increased the water in the atmosphere compared to the Eastern Pacific, rainfall was lower in the Western Pacific compared to the Eastern Pacific for equal amounts of water vapor in the atmospheric column — e.g., about 10mm / day in the Western Pacific, versus ~ 20mm / day in the Eastern Pacific at 55 mm water vapor, the peak of the distribution of water vapor amount
In Relationships between Water Vapor Path and Precipitation over the Tropical Oceans, Bretherton et al showed that although the
Western Pacific
warmer surface waters
increased the water
in the atmosphere compared to the Eastern Pacific, rainfall was lower in the Western Pacific compared to the Eastern Pacific for equal amounts of water vapor in the atmospheric column — e.g., about 10mm / day in the Western Pacific, versus ~ 20mm / day in the Eastern Pacific at 55 mm water vapor, the peak of the distribution of water vapor amount
in the atmosphere compared to the Eastern Pacific, rainfall was lower
in the Western Pacific compared to the Eastern Pacific for equal amounts of water vapor in the atmospheric column — e.g., about 10mm / day in the Western Pacific, versus ~ 20mm / day in the Eastern Pacific at 55 mm water vapor, the peak of the distribution of water vapor amount
in the
Western Pacific compared to the Eastern Pacific for equal amounts of water vapor
in the atmospheric column — e.g., about 10mm / day in the Western Pacific, versus ~ 20mm / day in the Eastern Pacific at 55 mm water vapor, the peak of the distribution of water vapor amount
in the atmospheric column — e.g., about 10mm / day
in the Western Pacific, versus ~ 20mm / day in the Eastern Pacific at 55 mm water vapor, the peak of the distribution of water vapor amount
in the
Western Pacific, versus ~ 20mm / day
in the Eastern Pacific at 55 mm water vapor, the peak of the distribution of water vapor amount
in the Eastern Pacific at 55 mm water vapor, the peak of the distribution of water vapor amounts.
Sea surface temperatures
in the
Western Pacific are well above climatology, and it has been argued that the warmth
in the
Western Pacific along with the lack of an equivalent long - term
warming trend
in the Eastern Pacific,
increase the chances of a «super El Niño,» comparable to the two strongest El Niños of the past century, which occurred
in 1998 and 1983.
«While La Niña [conditions
in 2011] had a large role to play
in the failure of the rains
in East Africa, there is evidence that
warming in the
western Pacific — Indian Ocean
warm pool has contributed to an
increased frequency of droughts
in this region,» the researchers note.
That being said, I recently critiqued a forestry paper that claimed global
warming is responsible for
increasing forest fire acreage
in the
Western U.S. here:
The AMV
warming also leads to reduced rainfall over the
western part of the US and Mexico and to a weak
increase in rainfall over Europe during boreal winter (see figure).
Hence, the projected regional
warming and consequent
increase in wildfire activity
in the
western United States is likely to magnify the threats to human communities and ecosystems, and substantially
increase the management challenges
in restoring forests and reducing greenhouse gas emissions.
They reported that «no catastrophic hurricane of category 4 or 5 intensity has made landfall
in the
Western Lake [northern Florida] area during the last 130 year documentary record» but «If future climatic changes, whether or not related to the anticipated greenhouse
warming, lead to a return of a «hyperactive» hurricane regime characteristic of the first millennium A.D., then the northeastern Gulf Coast is expected to experience a dramatic
increase in the frequency of strikes by catastrophic hurricanes.»
For
warming levels of 1 °C to 2 °C, the area burned by wildfire
in parts of
western North America is expected to
increase by 2 to 4 times for each degree (°C) of global
warming.»
With
increasing drought and higher temperatures
in the
western U.S. climate scientists worry about
increasing fire frequency by drying and
warming landscapes.
Indeed, the map at which JAXA spokesman Sasano was pointing (see photo above) had been expected by most experts to show that
western nations are to blame for substantial
increases in atmospheric levels of carbon dioxide, causing global
warming.
There may be as well a modest
increase of thermal energy
in the
western Pacific
warm pool.
During that same period, average annual rainfall
in New South Wales declined by 3.6 inches (92 millimeters).3 Scientists think the decline
in autumn rainfall
in southeast Australia since the late 1950s may be partly due to
increases in heat - trapping gases
in Earth's atmosphere.3, 14 Major bushfires over southeast Australia are linked to the positive phase of an ocean cycle called the «Indian Ocean Dipole» — when sea surface temperatures are
warmer than average
in the
western Indian Ocean, likely
in response to global
warming.15, 16
(5) explains the cause of the slowdown
in global
warming after around 2000 — cooling from
increased Eastern SO2 emissions offset the
warming caused by
Western Clean Air efforts, resulting
in a net slowdown
in the rate of decreasing global SO2 emissions.
See how global
warming increases the risk of forest fires
in western Siberia — and find other hot spots threatened by higher air temperature on the Climate Hot Map.
In regards to the first question, J. Stroeve (personal communication) notes that in the present warmer climate state, the tendency for a negative AO winter pattern to promote increased transport of ice into the western Beaufort / Chukchi seas — a pattern that historically has helped to reduce summer ice loss — actually enhances summer ice los
In regards to the first question, J. Stroeve (personal communication) notes that
in the present warmer climate state, the tendency for a negative AO winter pattern to promote increased transport of ice into the western Beaufort / Chukchi seas — a pattern that historically has helped to reduce summer ice loss — actually enhances summer ice los
in the present
warmer climate state, the tendency for a negative AO winter pattern to promote
increased transport of ice into the
western Beaufort / Chukchi seas — a pattern that historically has helped to reduce summer ice loss — actually enhances summer ice loss.
But many scientists believe the
increase in wildfires
in the
Western United States is partly the result of tinder - dry forests parched by
warming temperatures.
For example, mechanisms evaluated
in this work revealed a cooling trend
in Eurasia due to forest loss
in western North America; this finding, however, contrasts with evidence of a
warming trend
in the Northern Hemisphere high latitudes with
increased CO2 concentrations [45] that result
in shifts
in boreal forest range and disturbance regime [46].
While we can not assert with confidence whether this ongoing shift is part of natural ENSO variability or a manifestation of GHG - induced climate change [68], this
increase in variance coincides with rising temperatures
in the
Western Pacific
Warm Pool [23,69 — 71].
Recent years have seen a dramatic
increase in the simultaneous occurrence of extremely cold winter days
in the Eastern United States and extremely
warm winter days
in the
Western U.S., according to a new study.
Increasing drought frequency and
warming temperatures (fuel moisture) have also been positively associated with
increased wildfire activity, particularly
in Western North America [39,80 — 84].
Furthermore, with the recent
increases of late season hurricanes reaching the northeastern region of the United States, Irene
in 2011 and Sandy's recent landfall
in New Jersey on October 29, 2012 and the record breaking temperatures we are now seeing
in the
western United States where temperatures are reaching within a few degrees of the hottest recorded temperature on earth, 134 degrees Fahrenheit, are more evidence that the global climate is changing possibly due to global
warming.
Several studies focused on the Colorado River basin showed that annual runoff reductions
in a
warmer western U.S. climate occur through a combination of evapotranspiration
increases and precipitation decreases, with the overall reduction
in river flow exacerbated by human demands on the water supply.
What the report says about wildfires and climate change: The incidence of large forest fires
in the
western United States and Alaska has
increased since the early 1980s and is projected to further
increase as the climate
warms, with profound changes to certain ecosystems.
Since 1970, average annual temperatures
in the
Western U.S. have
increased by 1.9 ° F, about twice the pace of the global average
warming.
The
warming in Western Europe since about 1995 can be related to an
increase of about +1 °C of the surface temperature of the North Atlantic — following an equivalent cooling over 1970 - 1995 - and an
increase of the insolation with less aerosols.
As the climate changes
in response to global
warming, longer and more severe droughts are projected for the
western US The resulting dry conditions will
increase the pressure on groundwater supplies as more is pumped to meet demand even as less precipitation falls to replenish it.
http://www.sciencedaily.com/releases/2014/02/140202111055.htm «The satellite observations have shown that
warming of the tropical Indian Ocean and tropical
Western Pacific Ocean — with resulting
increased precipitation and water vapor there — causes the opposite effect of cooling
in the TTL region above the
warming sea surface.
As temperatures have
warmed, the prevalence and duration of drought has
increased in the
western U.S. and climate models unanimously project
increased drought
in the American Southwest.
The studies indicate that the observed pattern of mid-tropospheric
warming in recent decades over west central Asia led to an
increase in instability of the
western winds thereby
increasing WDs leading to a higher propensity for heavy precipitation over the
western Himalayas.
Scientists at IITM's Centre for Climate Change and Research R K Madhura, R Krishnan, Jayashree Revadekar, M Mujumdar and B N Goswami published their paper, «Changes
in western disturbances over
western Himalayas
in a
warming environment» which talks of the
increasing frequency of WDs — a low pressure system originating over the eastern Mediterranean sea and moves eastward.
The
increased mid-Holocene solar heating
in boreal summer leads to more
warming in the
western than
in the eastern Pacific, which strengthens the trade winds and inhibits the development of ENSO (Clement et al., 2000, 2004).
Trying to figure out the
increasing frequency of heavy precipitation over
western Himalayas, the scientists said their analysis suggested that pronounced
warming over the Tibetan plateau
in recent decades due to elevation dependency of climatic
warming signal favoured enhancement of meridianal temperature gradients.
Whether Global
Warming is real or not, it is clear that current
Western attempts to reduce CO2 emissions have achieved nothing but 1) Export their industry and jobs to India and China, 2)
Increase the CO2 emissions there above what they were in Europe, Australia and North America, so that total emissions increase, and 3) Massively increase domestic electricity prices while enriching Chinese Solar Panel and Wind Turbine manufa
Increase the CO2 emissions there above what they were
in Europe, Australia and North America, so that total emissions
increase, and 3) Massively increase domestic electricity prices while enriching Chinese Solar Panel and Wind Turbine manufa
increase, and 3) Massively
increase domestic electricity prices while enriching Chinese Solar Panel and Wind Turbine manufa
increase domestic electricity prices while enriching Chinese Solar Panel and Wind Turbine manufacturers.
Global
warming may
increase the frequency of intense hurricanes
in the
western Atlantic region during the 21st century.
«Indeed it is estimated that annual mean temperature has
increased by over 2 °C during the last 70 years and precipitation has decreased
in most regions, except the
western part of the country, indicating that Mongolia is among the most vulnerable nations
in the world to global
warming.»