Sentences with phrase «of upper level winds»

The case for a connection between Arctic warming and summertime extreme weather events rests on the Arctic's crucial role as a pacesetter and shapemaker of the jet stream, the powerful ribbon of upper level winds that steer weather systems from west to east across the Northern Hemisphere.

Not exact matches

Winds will be stronger at the upper stories of high - rise buildings, up to a full category above surface - level speeds.
Like Joby, these companies are exploiting new strong, cheap materials, advanced control electronics, and an improved understanding of upper - level wind patterns.
Water vapor seen at these infrared wavelengths is in the upper and middle levels of the troposphere, where the winds are ruled by large - scale air masses.
Every storm chase begins with an assessment of where supercells will burgeon, based on factors from the location of the so - called dry line — separating moist from arid air — to the speeds of upper - level winds.
The CTD sections show that the deeper layers are also warmer and slightly saltier and the observed sea level can be explained by steric expansion over the upper 2000 m. ENSO variability impacts on the northern part of the section, and a simple Sverdrup transport model shows how large - scale changes in the wind forcing, related to the Southern Annular Mode, may contribute to the deeper warming to the south.
These fast - moving bands of winds are found in the upper levels of the atmosphere and are created due to Earth's rotation, and its air being warmed up by solar radiation.
Over the Atlantic basin, the amplified trough is associated with stronger upper - level westerly winds and stronger lower - level easterly trade winds, both of which increase the vertical wind shear and suppress hurricane activity.
Light and variable upper - level winds in the vicinity of the storm are expected to remain light for the next few days, suggesting the system will meander in south Texas at least through Monday.
The home is well situated on the 10th Tee and takes advantage of the cooling trade winds felt throughout the home on both the upper and lower levels.
DESIGN AN ARTFUL BLEND OF ELEGANCE, COMFORT AND TRANQUILITY Two sumptuously furnished bedrooms, each with its own luxe master bath Spacious, fully equipped kitchen with granite countertops Top - of - the - line Sub-Zero and Viking appliances Comfortable outdoor living terrace and upper level balcony, perfect for entertaining with an awesome view Exquisite marble and solid hardwood flooring Vaulted ceilings with crown molding, natural native materials and old - world craftsmanship Wireless Internet (Wi - Fi) access and global Vonage phone service Panoramic ocean views with magnificent sunsets Outside your door, native stone walkways winding through stunning tropical landscapOF ELEGANCE, COMFORT AND TRANQUILITY Two sumptuously furnished bedrooms, each with its own luxe master bath Spacious, fully equipped kitchen with granite countertops Top - of - the - line Sub-Zero and Viking appliances Comfortable outdoor living terrace and upper level balcony, perfect for entertaining with an awesome view Exquisite marble and solid hardwood flooring Vaulted ceilings with crown molding, natural native materials and old - world craftsmanship Wireless Internet (Wi - Fi) access and global Vonage phone service Panoramic ocean views with magnificent sunsets Outside your door, native stone walkways winding through stunning tropical landscapof - the - line Sub-Zero and Viking appliances Comfortable outdoor living terrace and upper level balcony, perfect for entertaining with an awesome view Exquisite marble and solid hardwood flooring Vaulted ceilings with crown molding, natural native materials and old - world craftsmanship Wireless Internet (Wi - Fi) access and global Vonage phone service Panoramic ocean views with magnificent sunsets Outside your door, native stone walkways winding through stunning tropical landscape.
This decrease can be attributed to the El Nino that developed over the crucial autumn season, which favored a strengthening of the upper level westerlies over the tropical North Atlantic, increased tropical Atlantic wind shear, and a consequently less favorable environment for tropical cyclogenesis.
I made the connection, because some months ago, don't remember where, I read that strong «upper level winds» can actually, in some cases, intensify a thunderstorm, by increasing the strength of the updrafts within the cell.
The exact path, the upper level winds, the moisture content of the air: These all contribute to the strength of a cyclone.
We find robust relationships among seasonal and regional patterns of weaker poleward thickness gradients, weaker zonal upper - level winds, and a more meridional flow direction.
Extreme cold in the descending center low pressure of the lobe with potentially extreme warmth on the ascending side of course, with the lobes guiding the upper level winds.
Winds created aloft circulate around a large region of upper - level low pressure near each of the poles.
The major climate system indices that are operationally used at ICPAC include evolution of monsoons, medium and upper level winds, Madden - Julian Oscillation (MJO), Quasi Biennial Oscillation (QBO), El Niño Southern Oscillation, Indian Ocean dipole (IOD), tropical cyclones, sea surface temperature gradients among many others that have been derived from general circulation.
Climatology was aware of this decades ago as it became aware of changing variability, especially of mid-latitude weather, with changes in upper level winds.
In recent days, this area of low pressure has actually sagged to the southwest, which in turn has turned upper level winds more northwesterly than westerly over Maine.
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?
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.
There is generally one eastward wind layer and one westward layer at any given time: a new layer of eastward winds appears at upper levels once the previous eastward layer near the tropopause has been squeezed away by descending westward winds.
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