El Niño is most widely known for how it shifts
the location of warm ocean waters, leading to cooler - than - normal waters in the western tropical Pacific but warmer - than - normal in the central and eastern parts of the basin.
Not exact matches
I'd love to know what they did take into account in attempting to model that period — must include astronomical
location, sun's behavior, best estimates about a lot
of different conditions — where the continents were, what the
ocean circulation was doing, whether there had been a recent geological period that laid down a lot
of methane hydrates available to be tipped by Pliocene
warming into bubbling out rapidly.
As the locals might say, it's «claro» that Casa Clara has all the elements
of a perfect Riviera Maya vacation: panoramic
ocean views, airy rooms that let in
warm Caribbean breezes and a stellar
location across from sandy Playacar Beach.
Located in a sparsely populated gated community in Playa Negra, Casa Vista Azul is an unsurpassed
location for anyone who loves the
ocean, sun, sand, and the
warm gentle air
of the tropics.
A fluctuation in the
location of slightly
warmer surface water could hardly cause the global increase in
ocean heat content.
There is so little understanding about how the
ocean parses its response to forcings by 1) suppressing (local convective scale) deep water formation where excessive
warming patterns are changed, 2) enhancing (local convective scale) deep water formation where the changed excessive
warming patterns are co-located with increased evaporation and increased salinity, and 3) shifting favored deep water formation
locations as a result
of a) shifted patterns
of enhanced
warming, b) shifted patterns
of enhanced salinity and c) shifted patterns
of circulation which transport these enhanced
ocean features to critically altered destinations.
The size and
location of a large body
of warm water in the equatorial Pacific
Ocean drive the transition from El Nino to La Nina.
The ice sheet is the focus
of scientific research because its fate has huge implications for global sea levels, which are already rising as ice sheets melt and the
ocean warms, exposing coastal
locations to greater damage from storm surge - related flooding.
(07/08/2013)
Warmer ocean temperatures will increase the frequency and intensity
of tropical cyclones, typhoons and hurricanes in «most
locations» this century, concludes a new study based on simulations using six global climate models.
Climate change will affect fisheries and aquaculture through gradual
warming,
ocean acidification and through changes in the frequency, intensity and
location of extreme events.
As a result
of this juxtaposition
of cold air and
warm air, the eastern sides
of continents and the western fringes
of oceans in middle and high latitudes are the preferred
locations for extratropical storm development.
The study, published March 30 in the journal PLoS ONE, paves the way towards an important road map on the impacts
of ocean warming, and will help scientists identify the habitats and
locations where coral reefs are more likely to adapt to climate change.
Since that day at Pelican Cays, I have been fortunate to travel to many sites around the globe, ranging from the waters
of the southern Pacific
Ocean to the crashing surf along the Pacific coast
of North America, and what I see matches the observations made by what now is an army
of scientists: The Earth's flora and fauna are changing — shifting their geographic
locations, altering when they reproduce or dying wholesale — as a result
of human - induced global
warming.
This means that the
warmer the
oceans are near the
location of the glaciers or ice sheets, the more heavy oxygen there is in the ice core.
These partially offsetting effects lead to the expectation that direct human shifts in water storage on land will not have large effects on sea level in comparison to the effects
of ocean warming and mountain - glacier and ice - sheet melting (Wada et al., 2012), although notable uncertainties remain in regards to future groundwater use and reservoir construction, and these effects vary considerably depending on the specific
location (NRC, 2012e).
Further affirmation
of the reality
of the
warming is its spatial distribution, which has largest values at
locations remote from any local human influence, with a global pattern consistent with that expected for response to global climate forcings (larger in the Northern Hemisphere than the Southern Hemisphere, larger at high latitudes than low latitudes, larger over land than over
ocean).