A mesocosm experiment by scientists from GEOMAR Helmholtz Centre for Ocean Research Kiel, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research Bremerhaven (AWI) and the Institute for Baltic Sea Research Warnemünde (IOW) reveals for the first time
how ocean change might affect the special physical, chemical and biological characteristics of the ocean's uppermost boundary.
Not exact matches
It's strange
how quickly my mindset
changed from de-risking to increasing risk in two years, but I decided to take on $ 1,000,000 more in debt to buy a fixer in Golden Gate Heights because my online revenue was growing, my net worth had rebounded, and I strongly believed buying a panoramic
ocean view home on both levels for $ 720 / sqft was a no brainer.
Improving projections for
how much
ocean levels may
change in the future and what that means for coastal communities has vexed researchers studying sea level rise for years, but a new international study that incorporates extreme events may have just given researchers and coastal planners what they need.
«The Atlantic
Ocean surface circulation, and however that
changes, has implications for
how the rainfall
changes on continents.»
Since these set of
ocean currents are known to influence global climate, the researchers were interested to see if it correlated with rainfall in the Western Hemisphere, and
how such a correlation could
change over time.
There are clues that these species may fare better than their stony counterparts after a disaster, but more research needs to be done to understand
how storms, warming waters and
ocean acidification can alter the composition of reefs and whether these
changes are permanent or short - lived, Lasker says.
While the mission is already shedding new light on
how the field is
changing, this latest result focuses on the most elusive source of magnetism:
ocean tides.
Roger Haagmans, ESA's Swarm mission scientist, explained, «It's astonishing that the team has been able to use just two years» worth of measurements from Swarm to determine the magnetic tidal effect from the
ocean and to see
how conductivity
changes in the lithosphere and upper mantle.
One of the subtle
changes visible in the new data - set is
how the Amazon's greenness corresponds to one of the long - known causes of rainfall or drought to the Amazon basin:
changes in sea surface temperatures in the eastern Pacific
Ocean, called the El Nino Southern Oscillation.
In some locations, seismograms have been faithfully recording every shake in the Earth's crust for nearly a century, meaning geologists can dissect what Bromirski calls the «treasure trove» of archived paper drums — and find out
how ocean waves have
changed over the last 100 years.
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.
Researchers can measure annual
changes in
how the melt rate occurs, for example, or the effects of a single pulse of warm deep -
ocean water.
Reproductive isolation is the key to understanding
how new species form, and many types of barriers can divide a population and split it into two different groups: geographic (such as a mountain range, desert,
ocean or river), morphological (a
change in coloration, body type or reproductive organs), behavioral (a
change in breeding season, mating calls or courtship actions), and others.
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.
Changes in mass, rather than height, control
how the ice shelves and associated glaciers flow into the
ocean,» Paolo said.
How will climate
change affect the world's
oceans?
Timothy Lyons at the University of California, Riverside, and colleagues have worked out
how phosphate levels
changed in Earth's
oceans over the last 3 billion years by measuring the relative amounts of phosphorus in 700 samples from various rock formations around the world.
Yeh said the team's approach could also be used to study
how four or more pharmaceuticals interact, and a similar mathematical framework could be used to better understand climate
change (for example, to understand
how temperature, rainfall, humidity and acidity of the
oceans interact) and other scientific questions that have three or more key factors.
Models used to project conditions on an Earth warmed by climate
change especially need to consider
how the
ocean will move excess heat around, Legg said.
Greatly improved computer models began to suggest
how such jumps could happen, for example through a
change in the circulation of
ocean currents.
Comparing layers in the ice - core samples and
ocean sediments has allowed researchers to deduce e.g.
how the average temperature on Earth has
changed over time, and also
how great the variability was.
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.
The difference in lightning activity can't be explained by
changes in the weather, according to the study's authors, who conclude that aerosol particles emitted in ship exhaust are
changing how storm clouds form over the
ocean.
Sea - level rise and coral bleaching often dominate discussions about
how climate
change affects the
ocean, but a host of more subtle — and harder to research — trends also play a role in reshaping the world's marine ecosystems.
His discoveries have also revealed
how warming
ocean temperatures and acidification of
ocean water caused by climate
change lead to coral bleaching and death.
Next, Doney (p. 1512) reviews
how the chemistry of the
oceans is
changing, mostly due to human fossil fuel combustion, fertilizer use, and industrial activity.
On average, Antarctic sea ice may be considerably thicker than once thought, which could significantly
change how scientists assess sea ice dynamics and their interactions with the
ocean in a warming world.
By studying the chemistry of growth rings in the shells of the quahog clam, an international team led by experts from Cardiff University and Bangor University have pieced together the history of the North Atlantic
Ocean over the past 1000 years and discovered
how its role in driving the atmospheric climate has drastically
changed.
Two pieces examine
how climate
change is affecting marine biological systems: Schofield et al. (p. 1520) illustrate and discuss the role of
ocean - observation techniques in documenting
how marine ecosystems in the West Antarctic Peninsula region are evolving, and Hoegh - Guldberg and Bruno (p. 1523) present a more global view of the ways in which marine ecosystems are being affected by rapid anthropogenic variations.
So if researchers can chart the
changes in the number of salmon that swim upstream, they can get an accurate history of alterations in the
ocean — which gives evidence of
how climate has
changed over time.
Iron can fuel plankton blooms and influence
how the
ocean responds to climate
change, while the lead images show the impact of past pollution on the
ocean and continuing contamination in some parts of the world and aluminium is used as a tracer of desert dust inputs to the
ocean.
Gibson's recent paper, published in the journal Paleoceanography, contributes to a better understanding of just
how the
oceans reflect those rapid
changes.
Together, these pieces provide an introduction to some of the important discoveries we have made recently about our
oceans, underscore
how human activities are
changing them, and identify some of the challenges we must face if we are to continue to enjoy their vast but finite resources.
The chemistry in the growth rings in the shells of the clam — which occur much like the annual growth rings in the centre of trees — can act as a proxy for the chemical make - up of the
oceans, enabling researchers to reconstruct a history of
how the
oceans have
changed over the past 1000 years with unprecedented dating precision.
The results are extremely important in terms of discerning
how changes in the North Atlantic
Ocean may impact the climate and the weather across the Northern Hemisphere in the future.
Given the current dramatic rate of
change in the
ocean nitrogen cycle the researchers are not sure
how long it will take for marine ecosystems to adapt.
For scientific purposes, the Antarctic ice sheet is often divided into catchment basins so that comparative measurements can be taken to work out
how the ice in each basin is
changing and discharging ice to the
oceans.
Saba, who has conducted modeling studies on the impacts of climate
change on endangered leatherback turtles in the eastern Pacific
Ocean, says the Northwest Atlantic loggerhead study offers a new approach in understanding
how climate variability affects sea turtle populations.
While these results indicate that coccolithophore calcification might increase under future
ocean conditions, the researchers say that it's still unclear «whether, or
how, such
changes might affect carbon export to the deep sea.»
«The idea is that we can quantify materials in a sample of water that will give us a base line of
how the
ocean responds to climate
change and
ocean acidification,» Gallager said.
Foord and scientists at the University of Miami say the corals living in the shallow waters just south of Miami Beach may offer clues as to
how the world's disappearing coral can survive in
changing oceans.
Enter the toy octopus: A team of researchers in California is exploring
how the
changing ocean chemistry affects a hermit crab's fight - or - flight response by simulating octopus attacks in the laboratory.
Figure shows
how ocean currents
changes with temperature.
The team is trying to understand life history traits of benthos at the initial stage and the influence of
ocean currents in order to find out
how these organisms expand their habitat and respond to environmental
changes.
With so many instruments on the Yahtse, researchers have a unique opportunity to monitor
changes along the length of the glacier and discover
how, for example, local
changes in
ocean temperature and currents relate to movement further up the glacier.
He believes that no one has thought of combining the two theories before because it's not an intuitive idea to look at
how the effects of
changing patterns of
ocean circulation, which occur on time scales of thousands of years, would effect global silicate weathering, which in turn controls global climate on time scales of 100s of thousands of years.
But a
change in
how the anchoveta are handled could satisfy both the need to feed the Peruvian people and supply the fishmeal industry, Santiago de la Puente of the Institute for the
Oceans and Fisheries and colleagues note February 15 in Fish and Fisheries.
The working group on coupled biogeochemical cycling and controlling factors dealt with questions regarding the role of plankton diversity,
how ocean biogeochemistry will respond to global
changes on decadal to centennial time scales, the key biogeochemical links between the
ocean, atmosphere, and climate, and the role of estuaries, shelves, and marginal seas in the capturing, transformation, and exchange of terrestrial and open - marine material.
This new insight into
how the Southern
Ocean behaves will allow scientists to build computer models that can better predict
how our climate is going to
change in the future.
As Dr. Mackey cited in the published article Sea
Change: UCI oceanographer studies effects of global climate fluctuations on aquatic ecosystems: «They would tell us about upwelling and
how the
ocean wasn't just this one big, homogenous bathtub, that there were different water masses, and they had different chemical properties that influenced what grew there,» she recalls.