«Projecting electricity output at a wind farm is extraordinarily challenging as it involves predicting variable gusts and complex
wind eddies at the height of turbines, which are hundreds of feet above the sensors used for weather forecasting»
Wind energy: Projecting electricity output at a wind farm is extraordinarily challenging as it involves predicting variable gusts and complex
wind eddies at the height of turbines, which are hundreds of feet above the sensors used for weather forecasting.
The wind eddied and corkscrewed and whistled through its teeth at you.
Not exact matches
Temperature and pressure variations power
winds and storms, from minor
eddies to angry funnel clouds.
Until this research, a major uncertainty around the future impacts of climate change was whether the
eddy field would change with stronger
winds or whether it would remain static.
«To put this in some kind of context, if those small scale
eddies did not increase with
wind stress then the saturation of carbon dioxide in the Southern Ocean sink would occur twice as rapidly and more heat would enter our atmosphere and sooner.»
«If the
winds continue to increase as a result of global warming, then we will continue to see increased energy in
eddies and jets that will have significant implications for the ability of the Southern Ocean to store carbon dioxide and heat,» said Dr Hogg.
During the 12 - day at - sea experiment called GLAD (Grand Lagrangian Deployment), the research team deployed 300 GPS - equipped custom drifter soff the UM Rosenstiel School research vessel F.G. Walton Smith in a region where
wind - driven continental shelf currents mix with buoyancy - driven Mississippi River outflow currents and deep
eddy - driven currents in the Gulf of Mexico.
Lozier (p. 1507) discusses how recent studies have challenged our view of large - scale ocean circulation as a simple conveyor belt, by revealing a more complex and nuanced system that reflects the effects of ocean
eddies and surface atmospheric
winds on the structure and variability of the ocean's overturning.
And shear is important in generating «
eddies» — cyclonic or anticyclonic swirls of energy — within the overall
wind flow.
The
eddy lumbered past the northern side of Greenland, its
winds swirling clockwise.
A new study has found that turbulent mixing in the deep waters of the Southern Ocean, which has a profound effect on global ocean circulation and climate, varies with the strength of surface
eddies — the ocean equivalent of storms in the atmosphere — and possibly also
wind speeds.
Whipped up by surface
winds and girded by the Coriolis effect (produced by Earth's rotation),
eddies may grow to several hundred kilometers in diameter and are known to transport heat, chemicals and biology throughout the oceans» shallower depths.
The
eddies that pass over the East Pacific Rise are generated by westward
winds that come through mountain passes in Central America.
The scientists studied a specific type of turbulences known as synoptic
eddies, and calculated the total energy of their
wind speeds.
To definitively say that the birds are drafting off each other, however, the exact location of the
eddies and the areas of downdraft would need to be measured on ibises, which would require flying them in a
wind tunnel — a far more intrusive process than simply carrying a data logger.
A small cyclonic
eddy occurred within Wilhelmina Bay driven by strong, episodic southerly katabatic
winds (Figure 1a).
Maltrud, M.E., R.D. Smith, A.J. Semtner, and R.C. Malone, 1998: Global
eddy - resolving ocean simulations driven by 1985 — 1995 atmospheric
winds.
A few flakes first, in the dull gray late - afternoon sky, and then
wind - driven swirls and
eddies around the edges of their wide front porch.
A Catalina
eddy is rarely prolonged: as the heat over the deserts causes air to rise, the resulting pressure gradient and increase in the normal onshore
winds causes the vortex to dissipate.
Currently, up to nearly half of humanity's carbon dioxide output ends up dissolved in seawater, with most landing in the Southern Hemisphere oceans, where
wind - driven
eddies bury it deeply.
The corresponding working quasilinear wave equation for the barotropic azonal stream function Ψm ′ of the forced waves with m = 6, 7, and 8 (m waves) with nonzero right - hand side (forcing +
eddy friction) yields (34) u˜ ∂ ∂ x (∂ 2Ψm ′ ∂ x2 + ∂ 2Ψm ′ ∂ y2) + β˜ ∂ Ψm ′ ∂ x = 2Ω sin ϕ cos2 ϕT˜u˜ ∂ Tm ′ ∂ x − 2Ω sin ϕcos2 ϕHκu˜ ∂ hor, m ∂ x − (kha2 + kzH2)(∂ 2Ψm ′ ∂ x2 + ∂ 2Ψm ′ ∂ y2), [S3] where x = aλ and y = a ln -LSB-(1 + sin ϕ) / cos ϕ] are the coordinates of the Mercator projection of Earth's sphere, with λ as the longitude, H is the characteristic value of the atmospheric density vertical scale, T˜ is a constant reference temperature at the EBL, Tm ′ is the m component of azonal temperature at this level, u˜ = u ¯ / cos ϕ, κ is the ratio of the zonally averaged module of the geostrophic
wind at the top of the PBL to that at the EBL (53), hor, m is the m component of the large - scale orography height, and kh and kz are the horizontal and vertical
eddy diffusion coefficients.
TURBULANT FLOW; (
wind in surges,
eddies, chaotic flow, spkiy erratic velocity) Layer of hot air canopy gets MIXED and heat in the boudary escapes to the sky.
Eddy Turbine: The
eddy turbine is sleek in design, and is safe in
wind speeds up to 120 mph.
back to the horizontal gradient, if the upper tropospheric thermal
wind shear increase is greater than the decrease of the lower layer, then maybe the overall baroclinic instability would be stronger — but currently the upper level
eddy circulations do not transport much heat poleward, so would the structure of cyclones change so that a deeper layer of air is involved in the thermal advection, compensating for a weaker temperature gradient?
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Tropical cyclones seem to me to be a very good potential source of forcing «by daily and six - hourly
winds and heat fluxes», according to Enhanced vertical mixing within mesoscale
eddies due to high frequency
winds in the South China Sea [3]:
If the
wind field contains energy at the inertial frequency or higher (daily and six - hourly cases), then Vortex Rossby waves and near inertial waves are excited as ageostrophic expression of the vigorous
eddy field.
When a gyre region is added to the channel, vertical diffusion in the gyre exerts some control on the channel stratification even at higher
winds, forcing the mass balance into a mixed regime in which both
eddy and diffusive effects are important.
This behavior is expected if there is a baroclinic feedback that encourages the maximum baroclinic instability to be coincident with the maximum zonal
wind - speed, and discourages the meridional vacillation of the
eddy - driven jet stream.
Pilot balloon measurements during BoDEx point to a marked diurnal cycle in the
wind speed such that the LLJ accelerates over a near frictionless inversion by night but is mixed down to the surface by extreme radiative heating through modification of
eddy viscosity to produce a surface -
wind - speed maximum by ≈ 1100 local time (32).
The effects of mesoscale
eddies on the main subtropical thermocline are explored using a simply configured
wind - and buoyancy - driven primitive equation numerical model in conjunction with transformed Eulerian mean diagnostics and simple scaling ideas and closure schemes.