Not exact matches
Co-author Helen Russell (Institute of Astronomy, Cambridge, UK) expands: «The stars that form in the
wind close to the galaxy centre might
slow down and even start heading back inwards, but the stars that form further out in the
flow experience less deceleration and can even fly off out of the galaxy altogether.»
«The stars that form in the
wind close to the galaxy centre might
slow down and even start heading back inwards, but the stars that form further out in the
flow experience less deceleration and can even fly off out of the galaxy altogether,» said co-author Helen Russell, from the Institute of Astronomy at the University of Cambridge.
If the DNA branch (more THC - driven than
wind - driven) is
slowing down to reach 10 millions m3 / s, what is, for you, David, the
flow of GS near Florida?
The water piles up because the surface currents
flow slower than the
winds.
The June outlook reflects the fact that
winds during the last two weeks have reversed the
flow of the buoys and sea ice in the Beaufort Gyre and Transpolar Drift Stream,
slowing export and sequestering sea ice in the Arctic.
Much of it is forced down and it
flows back to the east at 200 metres depth and when the warm water surfaces at the Galapogos Islands in 9 months (replaceing the water which is
flowing east - west at the surface), it starts to
slow down the Trade
Winds because of the convection effect.
An array of turbines will have an effect on
wind flow similar to that of trees, they will
slow the
wind at lower levels due to the energy that they take from it and the turbulence that they cause.
When a
wind turbine takes energy from the
wind flowing through it, it
slows that
wind down.
Winds quickly drive CO2 away from the sunny regions where it is being released so it is easy to envisage Henry's Law applying in a particular location but if the CO2 rich air is being constantly removed then more outgassing can then occur in the same region and it is not hard to envisage an accumulation of CO2 downwind or over land masses where the
wind flow slows down.
For instance, since easterly
winds push water northwards and westerly
winds seawater southward, it is not obvious to non experts if a complete reversal of the westerlies blowing from N.America to Europe ought to make the gulf stream
flow slower or faster.
Two effects are identified that each contribute to a
slower eastward progression of Rossby waves in the upper - level
flow: 1) weakened zonal
winds, and 2) increased wave amplitude.
Enhanced warming of the Arctic affects the jet stream by
slowing its west - to - east
winds and by promoting larger north - south meanders in the
flow.