Not exact matches
These troughs
allow warmer and saltier waters from deeper in the
ocean to reach the glaciers and erode them.
RAPID RETREAT New seafloor data reveal that Køge Bugt (shown) and other fast - retreating glaciers in southeastern Greenland sit within deep fjords,
allowing warm Atlantic
Ocean water to speed up melting.
Any parts of the bed this low are easily exposed to
ocean water,
allowing the ice sheet to weaken from below as the
ocean water
warms.
Warm ocean waters, combined with little wind shear that could have torn the embryonic storm apart,
allowed...
This means the
warmer the
oceans become, the less able its inhabitants will be to boost their metabolism to between two and five times their resting metabolic rate, which is what
allows them to move, seek food and reproduce.
«The new data set will
allow us to check if our
ocean models can correctly represent changes in the flow of
warm water under ice shelves,» he added.
Perhaps extra carbon dioxide from a period of heightened seafloor eruptions eventually percolates through the
ocean and into the atmosphere,
allowing warming that would deliver a coup de grâce to the massive ice sheets.
«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.
This
allowed us to simulate a future climate scenario, characterized by both
warmer waters and
ocean acidification», explains researcher Christian Alsterberg.
If the water remained in the channel, the water would eventually cool to a point where it was not melting much ice, but the channels
allow the water to flow out to the open
ocean and
warmer water to flow in, again melting the ice shelf from beneath.
El Niños arrive every 3 to 7 years when winds fail in the tropical Pacific,
allowing warm water to pool in the eastern part of the
ocean.
B. Riegl and S. Purkis's E-Letter on our recent Review (1) focuses on promoting assisted migration, based on a belief that local adaptation and (unassisted) migration will be insufficient to
allow corals to cope with the effects of global
warming and
ocean acidification.
The discovery of genes involved in the production of DMSP in phytoplankton, as well as bacteria, will
allow scientists to better evaluate which organisms make DMSP in the marine environment and predict how the production of this influential molecule might be affected by future environmental changes, such as the
warming of the
oceans due to climate change.
Johnson hypothesizes that
warmer ocean temperatures in 2012 and 2013, which were 1.3 °C higher than the previous decade's average,
allowed the crabs to move north.
That could
allow heat from the
ocean to be released into the atmosphere — causing a jump in atmospheric global
warming, Trenberth says: «This could be a very important year.»
This means that even relatively small marine - protected areas could be effective in protecting the top - level predators and
allowing coral reefs to more fully recover from coral bleaching or large cyclones which are increasing in frequency due to the
warming of the
oceans as a result of climate change.
Some 5C of
warming appears to make the
Oceans less dense
allowing methane calthrates to be released from the
Ocean floor en masse.
«The southeast of Australia will experience
ocean warming that will
allow some fish species to move south into temperate waters,» he said.
Scientists believe climate change — the
warming of
oceans — has
allowed some of the almost 2,000 jellyfish species to expand their ranges, appear earlier in the year and increase overall numbers, much as
warming has helped ticks, bark beetles and other pests to spread to new latitudes.
Melting sea ice will mean
ocean currents can carry
warmer water and nutrients into Arctic water, taking fish further north and potentially
allowing them to mix between
oceans.
The longevity of global
warming (Fig. 9) and the implausibility of removing the
warming if it is once
allowed to penetrate the deep
ocean emphasize the urgency of slowing emissions so as to stay close to the 500 GtC target.
So if you can explain to me how the atmosphere could cause these three
oceans to
warm and
allow the rest to languish or cool, I would be very interested to hear it.
Reducing the heat lost to the atmosphere
allows the
oceans to steadily
warm over time - as has been observed over the last half century.
As I understand this article, the decrease in temp gradient in the cool skin layer is what
allows increases in atmospheric CO2 concentrations to further
warm the
oceans.
Located on the north coast, the
warm Caribbean waters lap at the soft sand that defines this appealing resort,
allowing visitors a place to relax in the sunshine or get active amid the fruitful
ocean.
Dalebrook is quieter (fewer people know about it), it has an outdoor shower, space to sit against the wall, a change room, and large boulders that
allow for skipping out into the pool before plunging into the Indian
ocean's slightly
warmer waters.
Buffalo City, as East London is charmingly known, not only lies on one of the most sublime coastlines of the world - think
warm Indian
Ocean waters and sub-tropical weather that
allow visitors to enjoy the climate all year round - it also basks gloriously between the Nahoon River in the north and the Buffalo River to the south of the city, and the phrase «unspoilt beaches» was termed with East London's beaches in mind.
Located on the eastern side of Mauritius, an island glimmering in the
warm currents of the Indian
Ocean, Blue Bay is protected by a vast coral reef that protects the beach from larger wave breaks,
allowing for calm, safe swimming.
Tucked away in Manuel Antonio, Costa Rica, SPA UNO
allows your body and mind to be soothed and rejuvenated while
warm ocean breezes and monkeys cascade through the rain forest.
Long, carefully thought out, and articulate discussions such as those found on Real Climate, Rabbett Run and Open Mind have
allowed me to remain confident in the scientific basis of concerns over global
warming and
ocean acidification (well sometimes Eli mystifies me).
Some 5C of
warming appears to make the
Oceans less dense
allowing methane calthrates to be released from the
Ocean floor en masse.
Some of the elements driving an increase in sea bottom
warming and methane release include: — increasingly ice free
ocean allowing more waves; — increasing (and increasingly intense?)
Understanding the gradient of the skin SST profile would also
allow us to under - stand how greenhouse gases
warm the
ocean.
That'd be a hint that
warm water could indeed get in under the icecap once the edges melt off, unblocking the deep channels and
allowing water to circulate in and out from the southern
ocean — wouldn't it?
This
warming is less than it will ultimately be, because the cool
ocean surface holds back the
warming —
allowing more energy loss out the bottom than will ultimately be the case.
In essence Zhang proposes that the
warming factors reduce the growth of sea ice which reduces
ocean overturning
allowing increased stratification of the
ocean which in turn reduces
ocean heat flux available to melt ice.
And, although I would love to claim that «
ocean» is my real name, the reason I am using a pseudonym is that anonymity
allows me more confidence in asking stupid questions because I am still on a learning curve with global
warming on other material discussed on RC.
This is a result of a weaker wind - driven
ocean circulation, when a large decrease in heat transported to the deep
ocean allows the surface
ocean to
warm quickly, and this in turn raises global surface temperatures.
The news service reports, «Scientists believe climate change — the
warming of
oceans — has
allowed some of the almost 2,000 jellyfish species to expand their ranges, appear earlier in the year and increase overall numbers, much as
warming has helped ticks, bark beetles, and other pests to spread to new latitudes.»
The increased area of
warm water on the surface
allows the tropical Pacific
Ocean to discharge more heat than normal into the atmosphere through evaporation.
One could argue that the
ocean is
warming due to loss of sea ice that
allows the
ocean to absorb more heat during the summer which carries over into the winter.
if it snows less when
oceans are cold and the arctic is closed, that has to
allow the sun to
warm the earth.
While there are some similarities between the approaches, an important difference is that the slab -
ocean approach
allows surface and MBL temperatures to adjust to the energetic perturbation: positive energetic forcing of the surface leads to
warming, weakens the inversion, and reduces low - cloud cover and liquid water path (LWP).
When the
oceans are cold and the Arctic is frozen, it does not snow much and that does
allow a decrease in ice albedo and earth does stop cooling and does start
warming.
By melting sea ice,
warming in the Arctic regions
allows more sunlight to be absorbed by the
ocean which leads to yet more
warming.
This is due to the twin drivers of an increasing land - sea thermal contrast, but more importantly,
warming over the Indian
Ocean which
allows more moisture to be carried to India.
On the other hand, if the
ocean is cooler than usual, clear morning skies last later into the day,
allowing increased
warming.
The measure of «climate» sensitivity by looking at only tropospheric temperature sensitivity might need to be examined a bit, especially, if turned out to be the case (as some research seems to indicate) that CO2 at 400 ppm induces a permanent La Niña state in the Pacific, while still
allowing for rapid
warming in other parts of the
ocean and climate system.
The persistent upwelling of cold water in the eastern tropical Pacific would have reduced cloud cover there, via reduced oceanic evaporation, and thus
allowed more of the sun's energy to enter the tropical
ocean - this would have aided the
ocean warming process, as generally the case when the tropical
ocean is cooler - than - normal.
How hurricanes develop also depends on how the local atmosphere responds to changes in local sea surface temperatures, and this atmospheric response depends critically on the cause of the change.23, 24 For example, the atmosphere responds differently when local sea surface temperatures increase due to a local decrease of particulate pollution that
allows more sunlight through to
warm the
ocean, versus when sea surface temperatures increase more uniformly around the world due to increased amounts of human - caused heat - trapping gases.25, 26,27,28