Not exact matches
One
study has estimated that UK imports of food products
and animal feed involved transportation by
sea,
air and road amounting to over 83 billion tonne - kilometres (3).
Nathaniel Johnson
and Shang - Ping Xie at the University of Hawaii
studied satellite
and rain - gauge data from the last 30 years
and found that
sea surface temperatures in the tropics now need to be about 0.3 °C higher than they did in 1980 before the
air above rises
and produces rain (Nature Geoscience, DOI: 10.1038 / ngeo1008).
«Through various theoretical, computational
and experimental
studies, we found that the mechanics of flapping propulsion are actually very similar in
air and in water,» said Kevin Chen, a graduate student in the Harvard Microrobotics Lab at
SEAS.
Previous
studies have suggested that Arctic
sea - ice loss causes the NAO to spend longer in its «negative phase» - generating more easterly winds that bring colder
air from Scandinavia
and Siberia to the UK.
The
study «The
Air -
Sea Interface
and Surface Stress Under Tropical Cyclones» was published in the June 16, 2014 issue of the journal Nature Scientific Reports.
Iron particles generated by cities
and industry are being dissolved by human - made
air pollution
and washed into the
sea — potentially increasing the amount of greenhouse gases that the world's oceans can absorb, a new
study suggests.
Study of upper ocean dynamics
and air -
sea interaction; investigation of the ocean's role in climate; sustained climate - quality observations in
and at the surface of the ocean; innovative ocean observations.
Kastak et al (2007 JASA)-- Aerial TTS
Study Onset, growth,
and recovery of in -
air temporary threshold shift (TTS) in a California
sea lion (Zalophus californianus).
You have your typical
air, land,
and sea units that develop
and improve with time
and study.
Our
studies did indicate that much of the heat entering the Barents
Sea in recent years was advected in by the inflow of warm Atlantic Waters and although direct warming through air - sea heat exchanges no doubt occurred, it appeared not be the dominate process at the time of our studi
Sea in recent years was advected in by the inflow of warm Atlantic Waters
and although direct warming through
air -
sea heat exchanges no doubt occurred, it appeared not be the dominate process at the time of our studi
sea heat exchanges no doubt occurred, it appeared not be the dominate process at the time of our
studies.
As an oceanographer working on
air /
sea interaction
and mixed layer dynamics, I hope I can clarify this issue somewhat (in fact, I'm at
sea right now on the R / P FLIP, gathering data to
study wave
and mixed layer dynamics, but this is off the point).
Intensive
and well - organized projects are usually an auspice of significant progress in the ocean - tropical cyclone
studies, such as the Coupled Boundary Layer
Air -
Sea Transfer (CBLAST)
and Impact of Typhoons on the Ocean in the Pacific (ITOP) projects.
Arctic
air temperatures are increasing at twice the rate of the rest of the world — a
study by the U. S. Navy says that the Arctic could lose its summer
sea ice by next year, eighty - four years ahead of the models —
and evidence little more than a year old suggests the West Antarctic Ice Sheet is doomed, which will add between twenty
and twenty - five feet to ocean levels.
Surface wind
and wave parameters at various scales help to describe the wind
and wave patterns in storms as well as to
study of
air -
sea interaction mechanisms in such energetic events.
«Not only is it extreme in any number of measures —
air temperature, loss of
sea ice
and on
and on — but there are so many things we haven't seen, particularly this extremely warm fall,» said
study co-author Brendan Kelly, executive director of the Study of Environmental Arctic Change at the University of Alaska, Fairb
study co-author Brendan Kelly, executive director of the
Study of Environmental Arctic Change at the University of Alaska, Fairb
Study of Environmental Arctic Change at the University of Alaska, Fairbanks.
Participants supported the development of an international
air -
sea flux working group sponsored by the Southern Ocean Observing System (SOOS) to coordinate the proposed pilot
study and oversee the task of defining flux requirements.
This
study differs from earlier research into possible links between hurricanes
and warmer
sea surface temperatures by looking as well at the effect of warmer
air.
Sea levels in the Indian Ocean are rising in some areas
and falling in others, which is at least partly a result of climate change influencing how the wind circulates
air above the surface of the ocean, said
study team member Weiqing Han, a climatologist at the University of Colorado in Boulder.
Lance, adrift in the ice, provided a base for 100 scientists
and engineers who spent 3 to 6 weeks on board the vessel
studying air - snow - ice - ocean interactions in a region with thinner
sea ice.
Develop
and validate retrieval algorithms for ocean
and sea ice parameters from various satellite Earth observation data, which in are used in
studies of upper layer mesoscale ocean processes,
air -
sea - ice interaction, climate change
studies and in operational oceanography.
And study authors found that 2 C to 5 C warming of local ocean waters with somewhat greater local air temperature increases was capable of flooding these basins in stages — forcing Totten's glacial ice to flow out into the Southern Ocean and provide significant contributions to sea level ri
And study authors found that 2 C to 5 C warming of local ocean waters with somewhat greater local
air temperature increases was capable of flooding these basins in stages — forcing Totten's glacial ice to flow out into the Southern Ocean
and provide significant contributions to sea level ri
and provide significant contributions to
sea level rise.
Several ocean -
air -
sea ice feedback processes may be operating (Meredith
and King 2005; Hanna 1996), though it has been difficult to pin down their relative roles in the observational
studies (King 1994; Jacobs
and Comiso 1997).
Our results point to the need for future observational
and modeling
studies to focus on the regional
and seasonal characteristics of Antarctic climate change, the regional response to ozone depletion, the influence of tropical variability
and climate change on Antarctic climate,
and on the mechanisms that link
sea ice
and air temperature in Antarctica.
A recent
study using archives from a polar - adapted forecast model found that West Antarctica is subject to frequent excursions of warm
and moist marine
air masses originating from the Ross
and Amundsen
Seas (Nicolas
and Bromwich 2010).
Here DeMott et al. work to fill in these knowledge gaps by reviewing published
studies dealing with observations of MJO processes, theories of
air -
sea interactions within the MJO,
and modeling
studies of these feedbacks.
The review
study found that high - resolution mixed layer ocean models can represent some of the complicated
air -
sea interactions
and recommended that scientists use coupled simulations
and evaluate them in terms of the observed relationship between convection
and sea surface temperature
and associated variables.
In addition, a
study commissioned by Canada's Fisheries
and Oceans Department examined the relationship between
air temperature
and sea ice coverage, concluding, «the possible impact of global warming appears to play a minor role in changes to Arctic
sea ice.»
Lo, 1997: Sensitivity of northern hemisphere
air temperatures
and snow expansion to North Pacific
sea surface temperatures in the Goddard Institute for Space
Studies general circulation model.
Blomquist B. W., S. E. Brumer, C. W. Fairall, B. J. Huebert, C. J. Zappa, I. M. Brooks, M. Yang, L. Bariteau, J. Prytherch, J. E. Hare, H. Czerski, A. Matei
and R. W. Pascal (October 2017): Wind Speed
and Sea State Dependencies of
Air -
Sea Gas Transfer: Results From the High Wind Speed Gas Exchange
Study (HiWinGS).
However, an assessment of transports at 48 ° N using five repeat World Ocean Circulation Experiment sections
and air -
sea heat
and freshwater fluxes as input to an inverse box model yielded no significant trend in the meridional overturning at that latitude (Lumpkin et al., 2008), though the time period
studied was relatively short (1993 - 2000).
Because Arctic
sea ice is influenced by both
air and water temperatures, the
study authors use a combination of Arctic ice core, tree - ring
and lake sediments to reconstruct Arctic conditions over the last 2,000 years.
Model
studies suggest that a collapse of the AMOC could lead to a reduction in surface
air temperature of around 1 - 3 °C in the North Atlantic region
and surrounding land masses, but with local cooling of up to 8 °C in areas of increased
sea ice (Vellinga
and Wood, 2002; Vellinga et al 2002; Manabe
and Stouffer; 1997; Jacob et al 2005).
These estimates resulted from
studies of
air bubbles recovered in ice cores from deep within Antarctica, Greenland
and other glaciers, as well as chemical analyses of coral samples from beneath the
sea.