Stott plans to investigate how
ocean warming led to a CO2 rise in the past, research that could also have implications for present climate change.
Not exact matches
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Changes in
ocean currents are also
lead to upwelling of
warm water, which also increases evaporation — and thus snow.
Willis is
leading a new mission to study the effects of
warming oceans on the melting of the Greenland Ice Sheet.
While it is still possible that other factors, such as heat storage in other
oceans or an increase in aerosols, have
led to cooling at the Earth's surface, this research is yet another piece of evidence that strongly points to the Pacific
Ocean as the reason behind a slowdown in
warming.
Coral bleaching is the most immediate threat to reefs from climate change; it's caused when
ocean temperatures become
warmer than normal maximum summer temperatures, and can
lead to widespread coral death.
«The undersides of glaciers in deeper valleys are exposed to
warm, salty Atlantic water, while the others are perched on sills, protected from direct exposure to
warmer ocean water,» said Romain Millan,
lead author of the study, available online in the American Geophysical Union journal Geophysical Research Letters.
Higher sea surface temperatures
led to a huge patch of
warm water, dubbed «The Blob,» that appeared in the northern Pacific
Ocean more than two years ago.
«This study focused on one single stressor,
ocean acidification, but we must keep in mind that the combination of several stressors, such as
ocean acidification and
warming could
lead to larger impacts on baby corals,» Dr Moya says.
The finding surprised the University of Arizona -
led research team, because the sparse instrumental records for sea surface temperature for that part of the eastern tropical Pacific
Ocean did not show
warming.
These large Northern Hemisphere cooling events have previously been linked to a change in the Atlantic
Ocean circulation that
led to a reduced transport of
warm water to the high latitudes in the North.
A new study
led by the University of Maryland's Earth System Science Interdisciplinary Center (ESSIC) suggests that a
warmer Atlantic
Ocean could substantially boost the destructive power of a future superstorm like Sandy.
Scientific observations show that in the Arctic,
warming temperatures have
led to a 75 % loss in sea ice volume since the 1980s, and recent reports suggest the Arctic
Ocean will be nearly free of summer sea ice by 2050, said Sullivan.
«Considering the Southern
Ocean absorbs something like 60 % of heat and anthropogenic CO2 that enters the ocean, this wind has a noticeable effect on global warming,» said lead author Dr Andy Hogg from the Australian National University Hub of the ARC Centre of Excellence for Climate System Sci
Ocean absorbs something like 60 % of heat and anthropogenic CO2 that enters the
ocean, this wind has a noticeable effect on global warming,» said lead author Dr Andy Hogg from the Australian National University Hub of the ARC Centre of Excellence for Climate System Sci
ocean, this wind has a noticeable effect on global
warming,» said
lead author Dr Andy Hogg from the Australian National University Hub of the ARC Centre of Excellence for Climate System Science.
Lead author, Dr Huw Griffiths from BAS says: «While a few species might thrive at least during the early decades of
warming, the future for a whole range of invertebrates from starfish to corals is bleak, and there's nowhere to swim to, nowhere to hide when you're sitting on the bottom of the world's coldest and most southerly
ocean and it's getting
warmer by the decade.»
«As the climate gets
warmer, the thawing permafrost not only enables the release of more greenhouse gases to the atmosphere, but our study shows that it also allows much more mineral - laden and nutrient - rich water to be transported to rivers, groundwater and eventually the Arctic
Ocean,» explained Ryan Toohey, a researcher at the Interior Department's Alaska Climate Science Center in Anchorage and the
lead author of the study.
A hotter atmosphere
warms the
oceans, which expand,
leading to sea level rise.
His discoveries have also revealed how
warming ocean temperatures and acidification of
ocean water caused by climate change
lead to coral bleaching and death.
A study
led by researchers at the University of Washington and the National Oceanic and Atmospheric Administration connects the unprecedented West Coast toxic algal bloom of 2015 that closed fisheries from southern California to northern British Columbia to the unusually
warm ocean conditions — nicknamed «the blob» — in winter and spring of that year.
«Combined with
warmer ocean temperatures throughout the year, this
leads to a longer growing season and faster plankton growth rates.
«For the first time we can quantify how
oceans responded to slow, natural climate
warming as the world emerged from the last ice age,» says Prof. Eric Galbraith from McGill University's Department of Earth and Oceanic Sciences, who
led the study.
They can also explain more than half of the
warming recorded over the Antarctic Peninsula, because «anomalously strong westerlies should act to decrease the incidence of cold air outbreaks from the south and
lead to increased
warm advection from the Southern
Ocean.»
Warmer air can carry more moisture, which can lead to more extreme rainfall events, and warmer ocean surface temperatures are known to intensify the most powerful hurri
Warmer air can carry more moisture, which can
lead to more extreme rainfall events, and
warmer ocean surface temperatures are known to intensify the most powerful hurri
warmer ocean surface temperatures are known to intensify the most powerful hurricanes.
«When we included projected Antarctic wind shifts in a detailed global
ocean model, we found water up to 4 °C
warmer than current temperatures rose up to meet the base of the Antarctic ice shelves,» said
lead author Dr Paul Spence from the ARC Centre of Excellence for Climate System Science (ARCCSS).
A new study
led by the University of Texas Institute for Geophysics has found that wind over the
ocean off the coast of East Antarctica causes
warm, deep waters to upwell, circulate under Totten Ice Shelf, and melt the fringes of the East Antarctic ice sheet from below.
At that time, changes in atmospheric - oceanic circulation
led to a stratification in the
ocean with a cold layer at the surface and a
warm layer below.
This interplay between climate and wind can
lead to sea level rise simply by moving water from one place in the
ocean to another, said Greene — no
warming of the air, or of
ocean temperatures required.
Dredging and sediment among the «stressors» Climate change is another threat, with
warming oceans likely to
lead to more extreme coral bleaching events, when corals lose the symbiotic algae that lend them their color.
Lead author, Dr Michael Singer from School of Earth and
Ocean Sciences at Cardiff University, said: «In drylands, convective (or short, intense) rainfall controls water supply, flood risk and soil moisture but we have had little information on how atmospheric
warming will affect the characteristics of such rainstorms, given the limited moisture in these areas.»
El Niño has helped to boost temperatures this year, as it
leads to
warmer ocean waters in the tropical Pacific, as well as
warmer surface temperatures in many other spots around the globe, including much of the northern half of the U.S..
Climate models do not predict an even
warming of the whole planet: changes in wind patterns and
ocean currents can change the way heat is distributed,
leading to some parts
warming much faster than average, while a few may cool, at least at first.
The list is long and familiar: too much carbon dioxide
warming the atmosphere and acidifying the
ocean; too much land being cleared,
leading to deforestation and desertification; overfishing causing crashes in one stock after another; and habitat destruction reducing biodiversity so drastically that some consider a sixth mass extinction to be under way.
In the study, the researchers use an ice -
ocean model created in Bremerhaven to decode the oceanographic and physical processes that could
lead to an irreversible inflow of
warm water under the ice shelf — a development that has already been observed in the Amundsen Sea.
Warming oceans can cause stress in coral,
leading them to expel the partner algae species they depend on for some of their food.
In general,
warmer ocean temperatures at the end of the Amazon's wet season
lead to reductions in rainfall and soil moisture at the beginning of the dry season.
«Such a slowdown is consistent with the projected effects of anthropogenic climate change, where
warming and freshening of the surface
ocean from melting ice caps
leads to weaker overturning circulation,» DeVries explained.
This research is part of a report on
ocean warming by some of the world's
leading climate change scientists.
«Loss of oxygen in the
ocean is one of the serious side effects of a
warming atmosphere, and a major threat to marine life,» said NCAR scientist Matthew Long,
lead author of the study.
Explosive volcanic eruptions in the tropics can
lead to El Niño events, those notorious
warming periods in the Pacific
Ocean with dramatic global impacts on the climate, according to a new study.
Coral skeletons are the building blocks of diverse coral reef ecosystems, which has
led to increasing concern over how these key species will cope with
warming and acidifying
oceans that threaten their stability.
«We found that where
ocean temperatures
warmed beyond a certain point as we neared the equator, at about 29 degrees, the pace of larval development slowed,» says study
lead author, Dr Ian McLeod.
Deep - sea oil exploration will probably release future spills, Solomon says, and global
warming could destabilize large undersea deposits of frozen methane,
leading to local
ocean acidification or oxygen depletion (SN 7/31/2010).
He is a
leading expert on climate cycles and the effects of global
warming on the Pacific
Ocean.
The deep circulation that drives
warm surface waters north is weakening,
leading to a cooling of the north Atlantic relative to the rest of the
oceans.
Dr Alison Cook, who
led the work at Swansea University, says: «Scientists know that
ocean warming is affecting large glaciers elsewhere on the continent, but thought that atmospheric temperatures were the primary cause of all glacier changes on the Peninsula.
The findings, published yesterday in the journal Nature, show that during the past 11,000 years, wind patterns have driven relatively
warm waters from the deep
ocean onto Antarctica's continental shelf,
leading to significant and sustained ice loss.
The paper's researchers,
led by U.C. Davis marine biologist Patrick Kilduff, explain that the NPGO — which is largely driven by a flavor of the El Niño Southern Oscillation (ENSO) that produces
warming in the tropical central Pacific
Ocean — has become more common in recent decades.
Warming oceans and melting land ice have caused
oceans to rise about seven inches since 1900, which has also
led to more frequent coastal flooding.
So recent
ocean cooling has
led some to conclude that global
warming has stopped.
These characteristics
lead to important differences in regional rates of surface
ocean warming that affect the atmospheric circulation.