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Find link is a tool written by Edward Betts.Longer titles found: Relative wind stress (view)
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Indian Monsoon Current
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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 oceanPortugal Current (600 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 inKelvin wave (1,386 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 anomaliesHenry Charnock (214 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" describesOcean dynamics (974 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 oceanAtlantic Equatorial mode (1,666 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 asPhysical oceanography (3,729 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 understandingSouthwest Madagascar Coastal Current (452 words) [view diff] exact match in snippet view article find links to article
high salinity characteristics of Subtropical Surface Waters. Driven by wind stress curl, the SMACC flows faster in summer and is reduced in winter, maintainingSubtropical 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 negativeEddy saturation and eddy compensation (1,519 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 sensitivityBrazil 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 theDownwelling (3,015 words) [view diff] exact match in snippet view article find links to article
transport is the net mass transport of the ocean surface resulting from wind stress and the Coriolis force. As wind blows across the ocean surface, it causesCritical depth (3,435 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 forGeorge Ridsdale Goldsbrough (929 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 intensificationMillennium 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 supportSlack tide (956 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 relationshipPelorus Sound (2,574 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 turbulenceAndaman Sea (4,290 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 oceanAngola–Benguela Front (2,262 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 ofTasman Sea (1,580 words) [view diff] exact match in snippet view article find links to article
Ocean. It transpires that while predominantly the location of westerly wind stress is a factor in how far north the formation of the Tasman Front occursADCIRC (1,064 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 theOcean observations (1,406 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)Chionoecetes (1,486 words) [view diff] exact match in snippet view article find links to article
column temperatures include increasing air temperature and northward wind stress. Warming trends on the outer Bering Sea shelf are concerning for a varietyArctic dipole anomaly (1,323 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..11011007WRoland Madden (1,099 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 theAlpine plant (2,561 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 increasedLake stratification (2,845 words) [view diff] exact match in snippet view article find links to article
radiation is distributed, which is why water turbulence, mainly caused by wind stress, can greatly increase the efficiency of heat transfer. In shallow lakesEquatorial wave (2,494 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 RossbyMindanao Current (1,671 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 MindanaoHarald Sverdrup (oceanographer) (1,174 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 SverdrupDwarf forest (3,414 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"Ocean current (3,837 words) [view diff] exact match in snippet view article find links to article
Australian Current, global warming has also been accredited to increased wind stress curls, which intensify these currents, and may even indirectly increaseTropical Ocean Global Atmosphere program (1,421 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 TheSea 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 waveHMS Conway (school ship) (2,905 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 perSea spray (3,330 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:Bodélé Depression (1,621 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 colocatedCyclone Global Navigation Satellite System (2,543 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 nearlyUpwelling (3,527 words) [view diff] no match in snippet view article find links to article
S2CID 31502815. Bakun, A; Nelson, CS (1991). "The seasonal cycle of wind-stress curl in subtropical eastern boundary current regions". Journal of PhysicalSverdrup 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 turbulenceSomali Current (2,937 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 alsoWind setup (943 words) [view diff] exact match in snippet view article find links to article
Coastal Engineering Smith, S.D. (1988). "Coefficients for sea surface wind stress, heat flux, and wind profiles as a function of wind speed and temperature"Wind generated current (1,395 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 principalPrindle, Patrick and Associates (1,493 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. TheYaquina Bay (4,432 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 withLong-period tides (1,625 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 InternationalPolar amplification (6,028 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 currentHeceta Bank (5,262 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 theClimate change in Saskatchewan (5,665 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 PanelSiri Kalvig (457 words) [view diff] exact match in snippet view article find links to article
(Vindstress på sjøis i Barentshavet)" (English: Local and micrometeorology (Wind stress on sea ice in the Barents sea)). Kalvig danced some ballet in her earlyNutrient cycling in the Columbia River Basin (7,083 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-relatedMarine biogeochemical cycles (10,775 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 waveLiquid 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 coastalAxel Timmermann (7,220 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 TimmermannEddy diffusion (7,924 words) [view diff] exact match in snippet view article find links to article
lost to smallest scales of motion. This is balanced mainly by tides and wind stress, which act as energy sources that continuously compensate for the dissipatedLatitude of the Gulf Stream and the Gulf Stream north wall index (2,340 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, 699-709Singular spectrum analysis (6,777 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, ASouthern Ocean overturning circulation (4,821 words) [view diff] exact match in snippet view article find links to article
brings water from the Circumpolar Deep Water (CDW) to the surface. Zonal wind stress induces upwelling near the pole and downwelling at the equator due to