Not exact matches
«Volcanic aerosols
in the stratosphere absorb infrared radiation, thereby heating up the stratosphere, and
changing the wind
conditions subsequently,» said Dr. Matthew Toohey, atmospheric scientist at GEOMAR Helmholtz Centre for
Ocean Research Kiel.
Now, a 15 - year, 30 - nation research collective called Geotraces is embarking on an ambitious global survey of
ocean chemistry to quantify trace elements and shed light on how chemical concentrations fluctuate
in response to
changing environmental
conditions.
However, while rangeomorphs were highly suited to their Ediacaran environment,
conditions in the
oceans continued to
change and from about 541 million years ago the «Cambrian Explosion» began — a period of rapid evolutionary development when most major animal groups first appeared
in the fossil record.
Back
in the lab, they will analyze the mosaics to see how the reefs are
changing over time, and how the variation of
ocean conditions and human activities impact each reef.
While Antarctic ice shelves are
in direct contact with both the atmosphere and the surrounding
oceans, and thus subject to
changes in environmental
conditions, they also go through repeated internally - driven cycles of growth and collapse.
These findings from University of Melbourne Scientists at the ARC Centre of Excellence for Climate System Science, reported
in Nature Climate
Change, are the result of research looking at how Australian extremes in heat, drought, precipitation and ocean warming will change in a world 1.5 °C and 2 °C warmer than pre-industrial condi
Change, are the result of research looking at how Australian extremes
in heat, drought, precipitation and
ocean warming will
change in a world 1.5 °C and 2 °C warmer than pre-industrial condi
change in a world 1.5 °C and 2 °C warmer than pre-industrial
conditions.
This
in turn
changes the prevailing winds to bring colder
conditions over the northern
oceans.
The rapid northerly shifts
in spawning may offer a preview of future
conditions if
ocean warming continues, according to the new study published
in Global
Change Biology by scientists from the Pacific States Marine Fisheries Commission, Oregon State University and NOAA Fisheries» Northwest Fisheries Science Center.
«
Changes in spawning timing and poleward migration of fish populations due to warmer
ocean conditions or global climate
change will negatively affect areas that were historically dependent on these fish, and
change the food web structure of the areas that the fish move into with unforeseen consequences,» researchers wrote.
It then fluctuated around that level, reaching a high of 306,220
in 2012 before declining below the carrying capacity
in the years since as
ocean conditions changed.
«These
conditions will cause
changes in phytoplankton growth and
ocean circulation around Antarctica, with the net effect of transferring nutrients from the upper
ocean to the deep
ocean,» said lead author J. Keith Moore, UCI professor of Earth system science.
The study, by an international team of scientists led by the University of Cambridge, examined how
changes in ocean currents in the Atlantic Ocean were related to climate conditions in the northern hemisphere during the last ice age, by examining data from ice cores and fossilised plankton sh
ocean currents
in the Atlantic
Ocean were related to climate conditions in the northern hemisphere during the last ice age, by examining data from ice cores and fossilised plankton sh
Ocean were related to climate
conditions in the northern hemisphere during the last ice age, by examining data from ice cores and fossilised plankton shells.
«The species lives
in habitats that are exposed to large
changes in ocean conditions and have limited scope to avoid these
changes.»
The results, published
in the journal Nature Geoscience, show how climate events
in the Northern Hemisphere were tightly coupled with
changes in the strength of deep
ocean currents in the Atlantic Ocean, and how that may have affected conditions across the g
ocean currents
in the Atlantic
Ocean, and how that may have affected conditions across the g
Ocean, and how that may have affected
conditions across the globe.
A team of biologists from the GEOMAR Helmholtz Centre for
Ocean Research Kiel, the Norwegian University of Science and Technology (NTNU) and the University of Florida has now been able to demonstrate with the comb jellyfish Mnemiopsis leidyi that, at least
in this type of jellyfish, the mechanism of regeneration can be
changed depending on the environmental
conditions.
«
Changes in ocean conditions that affect fish stocks, such as temperature and oxygen concentration, are strongly related to atmospheric warming and carbon emissions,» said author Thomas Frölicher, principal investigator at the Nippon Foundation - Nereus Program and senior scientist at ETH Zürich.
During the later period, when there was less sea ice, the whales dove significantly longer and deeper than
in the earlier period — presumably
in search of prey as the animals,
in turn,
changed their habits because of different
ocean conditions brought on by sea ice loss.
The findings presented at the Society of Marine Mammalogy's Biennial Conference
in San Francisco demonstrate that humpback foraging responds to environmental
changes, and illustrates how marine mammals serve as sentinels of ever -
changing ocean conditions.
As any sailor knows,
conditions at the
ocean's surface can
change in a moment.
(E) establishes performance measures for assessing the effectiveness of adaptation strategies intended to improve resilience and the ability of natural resources
in the coastal zone to adapt to and withstand the impacts of climate
change and
ocean acidification and of adaptation strategies intended to minimize those impacts on the coastal zone and to update those strategies to respond to new information or
changing conditions; and
In previous years, Antarctic sea ice hit record highs, potentially due to
changing ocean conditions linked to the melting of land - bound glaciers.
If we look into the
ocean, then
changes in the vertical temperature profiles may plausibly affect oceanic wave propagation, thus perturbing the
conditions to which the delayed mechanism is sensitive.
The open
ocean around the atoll was 2 degrees Celsius warmer than usual, but a short - term
change in weather
conditions pushed temperatures on top of the reef to 6 degrees Celsius above normal.
Because huge expanses of the deep
ocean will be exposed to
changing environmental
conditions as a result of climate
change (Mora et al., 2013; this study), the societal impacts of climate
change in the deep sea will undoubtedly be widespread, complex and dynamic.
Current
changes in the
ocean around Antarctica are disturbingly close to
conditions 14,000 years ago that new research shows may have led to the rapid melting of Antarctic ice and an abrupt 3 - 4 metre rise
in global sea level.
In the paper Gray makes many extravagant claims about how supposed changes in the THC accounted for various 20th century climate changes («I judge our present global ocean circulation conditions to be similar to that of the period of the early 1940s when the globe had shown great warming since 1910, and there was concern as to whether this 1910 - 1940 global warming would continu
In the paper Gray makes many extravagant claims about how supposed
changes in the THC accounted for various 20th century climate changes («I judge our present global ocean circulation conditions to be similar to that of the period of the early 1940s when the globe had shown great warming since 1910, and there was concern as to whether this 1910 - 1940 global warming would continu
in the THC accounted for various 20th century climate
changes («I judge our present global
ocean circulation
conditions to be similar to that of the period of the early 1940s when the globe had shown great warming since 1910, and there was concern as to whether this 1910 - 1940 global warming would continue.
This novel approach finds local populations
in the North Pacific and Northwest Atlantic are regionally synchronized and strongly correlated to
ocean conditions — such that climate models alone explain up to 88 % of the observed
changes over the past several decades.
The revolutionary discovery
in the 1970s of a thriving complex marine ecosystem around the hydrothermal vents of the Galapagos Rift on the
ocean floor of the eastern Pacific forever
changed our understanding of habitability showing that life could also arise and flourish
in the complete absence of sunlight
in conditions that were utterly toxic to any other life forms on Earth.
The researchers discovered that periods of increased radiative forcing could produce drought - like
conditions that extended indefinitely and that these
conditions were closely tied to prolonged
changes in Pacific
Ocean surface temperatures.
«Simply put, the shape of the ice sheet and the contact with the
ocean makes it likely that these areas respond more pronouncedly to
changes in climate boundary
conditions — be they atmospheric, oceanic or glaciological.»
California sea lions,
in particular, have been hit hard by
changing ocean conditions in recent years
in what has been called a «crisis.»
Life
in the
ocean is complex and
conditions change so quickly.
The
conditions of the
ocean in our Pacific Coast
change every 6 hours drastically from low tide to high tide.
The paleoclimate record (8.2 kyr, and earlier «large lake collapses») shows a dramatic drop
in surface temperatures for a substantial period of time when the
ocean circulation shuts off or
changes, but is that actually what would be expected under these warming
conditions?
It's killing fish, crabs and other marine life and leading researchers to believe that a fundamental
change may be taking place
in ocean conditions in the northern Pacific O
ocean conditions in the northern Pacific
OceanOcean.
There is not a single example of a simulation of the coupled
ocean - atmosphere - sea ice system that spontaneously generates a
change as big as doubling CO2,
in Holocene type
conditions.
If we look into the
ocean, then
changes in the vertical temperature profiles may plausibly affect oceanic wave propagation, thus perturbing the
conditions to which the delayed mechanism is sensitive.
The
oceans, which provide part of the boundary
conditions for the atmosphere, also have sufficient time to
change appreciably, and the
change in the oceanic state must be taken into account.
When Arctic researchers start investing
in floating buoys to study polar
ocean dynamics (instead of devices that sit on the sea ice), that's surely a sign of a sea
change in conditions and thinking.
What you guys will not come clean about however, is that these initial
conditions of the
ocean / atmosphere also impart a large range of uncertainty on multi-decadal predictions, even though you are invoking
changes in boundary values to gain skill.
Small
changes in initial
conditions drive abrupt and nonlinear
change evident
in many of the global
ocean and atmospheric indices — and indeed
in the surface temperature trajectory.
Here's a clue — a tendency toward a more frequent La Nina state, driven specifically by increasing GH gas concentrations (and similar to
conditions in the mid-Pliocene), may provide some modulation of tropospheric temperature spikes, but that energy will be advected somewhere (the idea of homogenous dispersion throughout the
ocean is absurd), and that somewhere is exactly where we are seeing the biggest
changes in the climate right now — the Arctic.
Whether
ocean circulation models... neither explicitly accounting for the energy input into the system nor providing for spatial variability
in the mixing, have any physical relevance under
changed climate
conditions is at issue.»
The accuracy of the data is questionable, the assumption of the initial
conditions questionable and comparing
oceans to land plus
oceans also would add uncertainty, but decreasing
ocean energy imbalance makes sense when you consider the
change in the rate of sea level rise.
Yet, we explained there is also reasonable basis for concern that a warming world may at least temporarily increase tornado damage including the fact that
oceans are now warmer, and regional
ocean circulation cycles such as La Nina / El Nino patterns
in the Pacific which affect upper atmospheric
conditions appear to becoming more chaotic under the influence of climate
change.
In some locations, changes in ocean temperatures and atmospheric patterns brought about by El Niño lead to drier conditions, which increases the damage during «fire season»
In some locations,
changes in ocean temperatures and atmospheric patterns brought about by El Niño lead to drier conditions, which increases the damage during «fire season»
in ocean temperatures and atmospheric patterns brought about by El Niño lead to drier
conditions, which increases the damage during «fire season».
Here a simple biologically and physically - based model of sapflow potential is used to assess observed
changes in sapflow across the Northeastern US from 1980 to 2006; document the correspondence between these observations and independent downscaled atmosphere
ocean general circulation model (AOGCM) simulations of
conditions during this period; and quantify
changes in sapflow potential through 2100.
(E) establishes methods for assessing the effectiveness of strategies and conservation actions taken to assist fish, wildlife, and plant populations, habitats, ecosystems, and associated ecological processes
in becoming more resilient, adapt to, and better withstand the impacts of climate
changes and
ocean acidification and for updating those strategies and actions to respond appropriately to new information or
changing conditions;
It seems unlikely that low level clouds — especially marine stratocumulous — would not respond to large scale
changes in ocean and atmospheric
conditions.
«The extreme winter of 2013/14 is
in line with historical trends
in wave
conditions and is also predicted to increasingly occur due to climate
change, according to some of the climate models, with the winter of 2015/16 also set to be among the stormiest of the past 70 years,» says Tim Scott, a lecturer
in ocean exploration at Plymouth University, and a co-author of the study.