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searching for Wind stress 49 found (77 total)

alternate case: wind stress

Indian Monsoon Current (1,027 words) [view diff] exact match in snippet view article find links to article

Somalia into the Bay of Bengal. These variations are due to changes in the wind stress associated with the Indian monsoon. The seasonally reversing open ocean
Portugal Current (601 words) [view diff] exact match in snippet view article find links to article
(averaging 177 days), particularly January and February, due to dominant wind stress along the Iberian margin, although upwelling can occasionally occur in
Kelvin wave (1,216 words) [view diff] exact match in snippet view article find links to article
often associated with anomalies in surface wind stress. For example, positive (eastward) anomalies in wind stress in the central Pacific excite positive anomalies
Henry Charnock (196 words) [view diff] exact match in snippet view article find links to article
meteorologist. He is well known for his work on surface roughness and wind stress over water surfaces. The now named "Charnock's relationship" describes
Ocean dynamics (972 words) [view diff] exact match in snippet view article find links to article
temperature, "S" is salinity, "g" is acceleration due to gravity, "τ" is wind stress, and "f" is the Coriolis parameter. "Q" is the heat input to the ocean
Southwest Madagascar Coastal Current (452 words) [view diff] exact match in snippet view article find links to article
high salinities characteristic of Subtropical Surface Waters. Driven by wind stress curl, the SMACC flows faster in summer and is reduced in winter, maintaining
Physical oceanography (3,686 words) [view diff] exact match in snippet view article find links to article
thermohaline circulation. Oceanic currents are largely driven by the surface wind stress; hence the large-scale atmospheric circulation is important to understanding
Eddy saturation and eddy compensation (1,476 words) [view diff] exact match in snippet view article find links to article
as proven by satellite altimetry. The relation between the increased wind stress and EKE is assumed to be near-linear, which explains the limited sensitivity
Atlantic Equatorial mode (1,663 words) [view diff] exact match in snippet view article find links to article
Atlantic basin, while a cool anomaly is associated with enhanced easterly wind stress in the same region. These trade wind fluctuations can be understood as
Subtropical Countercurrent (226 words) [view diff] exact match in snippet view article find links to article
warming makes the region conductive to atmospheric convection, and surface wind stress curls turn weakly positive along the front on the background of negative
George Ridsdale Goldsbrough (863 words) [view diff] exact match in snippet view article find links to article
planetary wave theory, Sverdrup's 1947 theory relating the curl of the wind stress to meridional transport, and Stommel's 1948 theory of the westward intensification
Brazil Current (766 words) [view diff] exact match in snippet view article find links to article
has low transport then the path of the Brazil Current is dominated by wind stress curl. However, if the Falkland Current transport is increased then the
Millennium Tower (Tokyo) (330 words) [view diff] exact match in snippet view article
earthquakes and hurricane-strength winds, the shape is aerodynamic to reduce wind stress, and helical bands are wrapped around the tower for structural support
Critical depth (3,424 words) [view diff] exact match in snippet view article find links to article
mixing for spring bloom initiation. By assigning varying values for wind stress and surface heat flux, they were able to develop parameterizations for
Slack water (946 words) [view diff] exact match in snippet view article find links to article
reverses, thus altering the time and duration of slack water. Variations in wind stress also directly affect the height of the tide, and the inverse relationship
Andaman Sea (4,079 words) [view diff] exact match in snippet view article find links to article
of up to 7.2 metres (24 ft). The effect of wind stress on the ocean surface can be explained by wind stress curl. The net divergence of water in the ocean
ADCIRC (1,020 words) [view diff] exact match in snippet view article find links to article
seafloor composition), as well as utilize atmospheric forcing data (wind stress and atmospheric pressure) from several sources, and further reduce the
Pelorus Sound (2,568 words) [view diff] exact match in snippet view article find links to article
the steep topography. Wind stress acting on the surface generates currents, which have not been well described. The wind stress also generates turbulence
Angola–Benguela Front (2,288 words) [view diff] exact match in snippet view article find links to article
north-flowing cold water of the Benguela current and the associated surface wind stress. However, Meeuwis and Lutjeharms (1990) concluded that the position of
Ocean observations (1,408 words) [view diff] exact match in snippet view article find links to article
fluxes Surface thermodynamic fluxes Wind speed and direction Surface wind stress Water vapor Sea surface temperature (SST) Sea surface salinity (SSS)
Arctic dipole anomaly (1,317 words) [view diff] exact match in snippet view article find links to article
1175/2758.1. Watanabe, E.; Hasumi, H. (2005). "Arctic sea ice response to wind stress variations". J. Geophys. Res. 110 (C11): C11007. Bibcode:2005JGRC..11011007W
Alpine plant (2,387 words) [view diff] exact match in snippet view article find links to article
occur, it normally happens to plants growing on exposed sites, where wind stress is increased. Alpine plants avoid water loss by deep rooting and increased
Roland Madden (1,094 words) [view diff] exact match in snippet view article find links to article
atmospheric carbon dioxide; The first estimates relating MJO tropical wind stress and the rotation of the earth; The first quantitative measures of the
Harald Sverdrup (oceanographer) (1,091 words) [view diff] no match in snippet view article
ocean circulation postulating a dynamical vorticity balance between the wind-stress curl and the meridional gradient of the Coriolis parameter, the Sverdrup
Equatorial wave (2,491 words) [view diff] exact match in snippet view article find links to article
waves), KT is temperature diffusion, KE is eddy diffusivity, and τ is the wind stress in either the x or y directions. Primitive equations Beta plane Rossby
Mindanao Current (1,619 words) [view diff] exact match in snippet view article find links to article
the extreme topography of the region, and complicating factors such as wind stress fluctuations and eddies. The most extensive observations of the Mindanao
Dwarf forest (3,368 words) [view diff] case mismatch in snippet view article find links to article
doi:10.2307/2989784. JSTOR 2989784. Lawton, Robert O. (September 1982). "Wind Stress and Elfin Stature in a Montane Rain Forest Tree: An Adaptive Explanation"
Tropical Ocean Global Atmosphere program (1,416 words) [view diff] exact match in snippet view article find links to article
Mechanisms that organize convection Oceanic response to combined buoyancy and wind stress forcing Atmospheric/oceanic interactions that impact other regions The
Sea spray (3,227 words) [view diff] exact match in snippet view article find links to article
(2012-07-03). "The wave state and sea spray related parameterization of wind stress applicable from low to extreme winds". Journal of Geophysical Research:
Upwelling (3,518 words) [view diff] no match in snippet view article find links to article
PMID 14726595. Bakun, A; Nelson, CS (1991). "The seasonal cycle of wind-stress curl in subtropical eastern boundary current regions". Journal of Physical
Sea salt aerosol (1,024 words) [view diff] exact match in snippet view article find links to article
common cause is the bursting of air bubbles, which are entrained by the wind stress during the whitecap formation. Another is tearing of drops from wave
Polar amplification (3,251 words) [view diff] no match in snippet view article find links to article
the Antarctic Circumpolar Current (ACC). Eventually, upwelling due to wind-stress transports cold Antarctic waters through the Atlantic surface current
HMS Conway (school ship) (2,884 words) [view diff] exact match in snippet view article
the Southwest Residual, a dynamic reaction which directly reflects wind stress in the Irish Sea. The north-westerly mean wind speed of 16 meters per
Cyclone Global Navigation Satellite System (2,494 words) [view diff] exact match in snippet view article find links to article
radars, by detecting changes in surface roughness caused by near surface wind stress. The quality of the measurements is determined by comparisons to nearly
Somali Current (3,086 words) [view diff] no match in snippet view article find links to article
formation of the Great Whirl is a response to the very strong anti-cyclonic wind-stress curl". Since the Somali current changes seasonally, the Great Whirl also
Sverdrup Gold Medal (1,464 words) [view diff] exact match in snippet view article find links to article
based on nonlinear, three-dimensional models of the oceans driven by wind stress and differential heating. 1971 Klaus Hasselmann for his work on turbulence
Bodélé Depression (1,660 words) [view diff] exact match in snippet view article find links to article
Contemporary deflation from the Bodélé is delineated by topography, such that wind stress, the maximum in dust output and the topographic depression are colocated
Wind generated current (1,454 words) [view diff] exact match in snippet view article find links to article
wind. The reverse effect applies to the polar gyres – the sign of the wind stress curl and the direction of the resulting currents are reversed. The principal
Prindle, Patrick and Associates (1,367 words) [view diff] exact match in snippet view article find links to article
designs in East Volusia, Florida, however. The roofs failed hurricane wind stress tests, and the heating and air conditioning systems often failed. The
Yaquina Bay (4,410 words) [view diff] exact match in snippet view article find links to article
DO levels of imported ocean water are dependent on physical factors (wind stress and cool water temperature) and biological factors (association with
Long-period tides (1,623 words) [view diff] exact match in snippet view article find links to article
P.; Chao, Benjamin Fong; Zheng, Dawei; Au, Andrew Y. (2000-08-01). "Wind stress forcing of the North Sea 'pole tide'". Geophysical Journal International
Heceta Bank (5,264 words) [view diff] exact match in snippet view article find links to article
up to the surface along the coastline due to the dominant southward wind stress on the coastal waters. The upwelled water brings nutrients up to the
Climate change in Saskatchewan (5,650 words) [view diff] exact match in snippet view article find links to article
aggregated. Deformities of individual trees is also likely to be seen due to wind stress from colonizing the open tundra. According to the Intergovernmental Panel
Marine biogeochemical cycles (10,753 words) [view diff] exact match in snippet view article find links to article
common cause is the bursting of air bubbles, which are entrained by the wind stress during the whitecap formation. Another is tearing of drops from wave
Nutrient cycling in the Columbia River Basin (7,036 words) [view diff] exact match in snippet view article find links to article
1016/j.dsr2.2004.12.023. Pierce, S.D.; Barth, J. A. (2017). "Wind stress, cumulative wind stress, and spring transition dates: data products for Oregon upwelling-related
Liquid Jungle Lab (2,439 words) [view diff] exact match in snippet view article find links to article
physiographic gap in the central mountain range which divides the Isthmus. This wind stress creates seasonal Ekman spiral pumping and displaces nutrient-poor coastal
Axel Timmermann (7,150 words) [view diff] exact match in snippet view article find links to article
FF Jin, M Collins, Geophysical Research Letters 31 (12), 2004 Is the wind stress forcing essential for the meridional overturning circulation?, A Timmermann
Latitude of the Gulf Stream and the Gulf Stream north wall index (2,339 words) [view diff] no match in snippet view article find links to article
Behringer, D., L. Regier and H. Stommel. (1979). "Thermal feedback on wind-stress as a contributing cause of the Gulf Stream", J. Mar. Res., 37, 699-709
Singular spectrum analysis (6,757 words) [view diff] exact match in snippet view article find links to article
North Atlantic ocean's temperature field and its association with the wind stress forcing", Journal of Climate, doi:10.1175/jcli-d-16-0370.1. Groth, A