While more extreme storms and rising sea levels are some of
the impacts of warmer oceans, rising CO2 levels and the resulting warmer oceans are impacting ocean health itself.
Many reefs, from islands in the South Pacific to the Florida Keys, have felt
the impacts of the warmer oceans.
Not exact matches
In the current context
of global
warming it is important to assess the
impacts that changes in
ocean and climate may have on Antarctica, and reconstructing past climate fluctuations provides vital information on the responses and possible feedback mechanisms within the climate system.
«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.
Koslow has researched the
impact of climate - change - driven
warming on what are known as oxygen minimum zones (OMZs), naturally occurring low - oxygen regions found well below the
ocean's surface.
In this regard, one
of the key questions is: How will the
warming of the
oceans and resultant decrease in dissolved oxygen
impact marine life forms» productivity?
The extensive methane seep mounds across the remote arctic island
of Ellef Ringnes may be a caution from the past regarding potential
impacts of modern
warming of the Arctic
Ocean.
One
of the biggest lingering issues in the global
warming slowdown is the full
impact of the natural temperature cycles
of Earth's
oceans.
Similar frozen methane hydrates occur throughout the same arctic region as they did in the past, and
warming of the
ocean and release
of this methane is
of key concern as methane is 20x the
impact of CO2 as a greenhouse gas.
New research into the
impact of climate change has found that
warming oceans will cause profound changes in the global distribution
of marine biodiversity.
Taylor and her colleagues also tested water temperature and pH levels in the laboratory to study the
impact of ocean warming and acidification on the exoskeletons
of several species
of crustacean.
The projected
impacts of a
warming atmosphere and
oceans on the Earth's hydrological cycle — dry regions likely becoming drier, while wet ones become more wet — will likely exacerbate this already dire situation.
Retreating sea ice in the Iceland and Greenland Seas may be changing the circulation
of warm and cold water in the Atlantic
Ocean, and could ultimately
impact the climate in Europe, says a new study by an atmospheric physicist from the University
of Toronto Mississauga (UTM) and his colleagues in Great Britain, Norway and the United States.
Changes to Antarctic winds have already been linked to southern Australia's drying climate but now it appears they may also have a profound
impact on
warming ocean temperatures under the ice shelves along the coastline
of West and East Antarctic.
Unexpectedly, this more detailed approach suggests changes in Antarctic coastal winds due to climate change and their
impact on coastal currents could be even more important on melting
of the ice shelves than the broader
warming of the
ocean.
At a global scale, the increased melting
of the ice sheet contributes to rising sea level and may
impact global
ocean circulation patterns through the so - called «thermohaline circulation'that sustains among others, the Gulf Stream, which keeps Europe
warm.
The area boasts the world's
warmest ocean temperatures and vents massive volumes
of warm gases from the surface high into the atmosphere, which may shape global climate and air chemistry enough to
impact billions
of people worldwide.
It's unclear whether this year's strong El Niño event, which is a naturally occurring phenomenon that typically occurs every two to seven years where the surface water
of the eastern equatorial Pacific
Ocean warms, has had any
impact on the Arctic sea ice minimum extent.
Predicting the
impact of climate change on ecological communities is tricky, but predicting the
impact of El Niño, the cyclical
warming in the Pacific
Ocean that affects temperature and rainfall around the globe, is even trickier.
«Atlantic / Pacific
ocean temperature difference fuels US wildfires: New study shows that difference in water temperature between the Pacific and the Atlantic
oceans together with global
warming impact the risk
of drought and wildfire in southwestern North America.»
«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.
«The Earth is in the midst
of a biodiversity crisis,» Sorte said, «and the Gulf
of Maine is one
of the fastest -
warming areas
of the global
ocean, so the
impacts of ocean warming are likely to happen much sooner there.»
That figure will rapidly increase each year as
warmer temperatures thin permafrost, Peter Wadhams, a professor
of ocean physics at the University
of Cambridge and co-author
of the economic
impact study, wrote in an e-mail.
Coral reefs, which support diverse communities
of fish and other marine life, are declining globally at unprecedented rates due to human - caused
impacts, such as
warming waters and
ocean acidification.
Scientists have discovered that rising
ocean temperatures slow the development
of baby fish around the equator, raising concerns about the
impact of global
warming on fish and fisheries in the tropics.
He and his colleagues hope to find correlations between those circumstances and diversity, which might enable them to predict the
impact of global
warming and the resulting
ocean acidification on marine ecosystems.
«However, the recent climate anomalies as a result
of climate change and
warming of the Atlantic
Ocean have created severe droughts in the tropics, causing major
impacts on forests.»
While El Niño is a cyclical climate phenomenon in the Pacific
Ocean — marked by warmer ocean temperatures in the tropics and a weakening of the usual easterly trade winds — it can impact weather around the g
Ocean — marked by
warmer ocean temperatures in the tropics and a weakening of the usual easterly trade winds — it can impact weather around the g
ocean temperatures in the tropics and a weakening
of the usual easterly trade winds — it can
impact weather around the globe.
They will also hear from researchers looking at issues associated with
ocean warming and acidification and associated
impacts of coral reefs.
Most also recognize that such global agreements are the most difficult to come by, and that local protection strategies and efforts to reduce stressors on corals and marine life are important steps in at least staving off the
impacts of ocean acidification and global
warming.
Significant changes in the circulation
of the
ocean could likewise
impact fisheries in the United States that can be devastated by
warming waters, thereby affecting livelihood and food source.
Projected
impacts of global
warming and
ocean acidification motivated this action, but as marine biologist Ayana Elizabeth Johnson eloquently writes in a New York Times op - ed: «climate change really is only half the story.»
That's weakening coral reefs around the world, making them more vulnerable to
impacts of ocean warming and water pollution.
Extraction
of the excess CO2 from the air in this case would be very expensive and perhaps implausible, and
warming of the
ocean and resulting climate
impacts would be practically irreversible.
«The 2 °C target was all about
warming and didn't involve consideration
of ocean acidification in any direct way,» said University
of Queensland professor Ove Hoegh - Guldberg, one
of the lead authors
of the recent Intergovernmental Panel on Climate Change assessment chapter dealing with
ocean impacts.
A reduction
of regional stress such as nutrient runoff or the loss
of oxygen can mitigate the
impact of global stressors like
ocean acidification and
warming.
Warm ocean waters that sucked the color and vigor from sweeping stretches
of the world's greatest expanse
of corals last month were driven by climate change, according to a new analysis by scientists, who are warning
of worse
impacts ahead.
According to Laura Sherr, a Marine Mammal Center spokeswoman, besides toxins,
warming ocean temperatures have also had an
impact on a harbor seal mother's ability to forage for food to take care
of their pups.
[1] CO2 absorbs IR, is the main GHG, human emissions are increasing its concentration in the atmosphere, raising temperatures globally; the second GHG, water vapor, exists in equilibrium with water / ice, would precipitate out if not for the CO2, so acts as a feedback; since the
oceans cover so much
of the planet, water is a large positive feedback; melting snow and ice as the atmosphere
warms decreases albedo, another positive feedback, biased toward the poles, which gives larger polar
warming than the global average; decreasing the temperature gradient from the equator to the poles is reducing the driving forces for the jetstream; the jetstream's meanders are increasing in amplitude and slowing, just like the lower Missippi River where its driving gradient decreases; the larger slower meanders increase the amplitude and duration
of blocking highs, increasing drought and extreme temperatures — and 30,000 + Europeans and 5,000 plus Russians die, and the US corn crop, Russian wheat crop, and Aussie wildland fire protection fails — or extreme rainfall floods the US, France, Pakistan, Thailand (driving up prices for disk drives — hows that for unexpected adverse
impacts from AGW?)
However, this in itself is not enough to define what level
of warming is «dangerous,» especially since the projections
of actual
impacts for any level
of warming are highly uncertain, and depend on further factors such as how quickly these levels are reached (so how long ecosystems and society have had to respond), and what other changes are associated with them (eg: carbon dioxide concentration, since this affects plant photosynthesis and water use efficiency, and
ocean acidification).
Geoengineering proposals fall into at least three broad categories: 1) managing atmospheric greenhouse gases (e.g.,
ocean fertilization and atmospheric carbon capture and sequestration), 2) cooling the Earth by reflecting sunlight (e.g., putting reflective particles into the atmosphere, putting mirrors in space to reflect the sun's energy, increasing surface reflectivity and altering the amount or characteristics
of clouds), and 3) moderating specific
impacts of global
warming (e.g., efforts to limit sea level rise by increasing land storage
of water, protecting ice sheets or artificially enhancing mountain glaciers).
Fourteen research teams studying the
impacts of warming on the Arctic
Ocean have issued independent projections
of how the sea ice will behave this summer, and 11
of them foresee an ice retreat at least as extraordinary as last year's or even more dramatic.
Updated, Nov. 10, 2015, 3:04 p.m. A new study in Nature Climate Change, «Revaluating
ocean warming impacts on global phytoplankton,» has shown that the method used to calculate phytoplankton loss in the 2010 research greatly overstated plankton losses because
of a missing vital factor.
It discusses the only the
impact of the
ocean on rates
of warming and how that reduced expected trends in Antarctica with respect to earlier simulations that did not include such effects.
We often see «skeptics» suggest that the additional
warming stored in the
ocean can't possibly come back to affect tropospheric temperatures in any meaningful way, but the record levels
of energy being stored in the Indo Pacific
Warm Pool has
impacted and made possible the record tropospheric temperatures Australia saw in 2013.
«Others have identified the lags in the southern
ocean (which
warms more slowly than the northern hemisphere, and northern land in particular) as the source
of this time dependence
of feedbacks, and we've demonstrated that different forcings have subtly different
impacts — `
There are continuing major questions about the future
of the great ice sheets
of Greenland and West Antarctica; the thawing
of vast deposits
of frozen methane; changes in the circulation patterns
of the North Atlantic; the potential for runaway
warming; and the
impacts of ocean carbonization and acidification.
«The fact that we are seeing an expansion
of the
ocean's least productive areas as the subtropical gyres
warm is consistent with our understanding
of the
impact of global
warming,» he said.
Others have identified the lags in the southern
ocean (which
warms more slowly than the northern hemisphere, and northern land in particular) as the source
of this time dependence
of feedbacks, and we've demonstrated that different forcings have subtly different
impacts — to some extent based on their spatial signatures.
However, albedo modification would only temporarily mask the
warming effect
of greenhouse gases and would not address atmospheric concentrations
of CO2 or related
impacts such as
ocean acidification.