Both its physical properties and its rate and direction of motion are influenced by a variety of factors, including solar radiation, the geographic position of continents, ocean currents, the location and orientation of mountain ranges, atmospheric chemistry, and vegetation growing on the land surface.
appalachiantrail.com Exploring a series of atmospheric mountain villages – staying in basic guesthouses, or gîtes – is easy from the town of Imlil, about 90 minutes from Marrakech.
Elsewhere were several varieties of the ambitious new folk, including Lord Huron's atmospheric mountain music, the intimate traditionalism of Shovels & Rope and the whimsy of Of Monsters and Men (less so, the deeply inert Lumineers).
Mt. Cimone is the highest peak of the northern Italian Apennines and is the only high mountain station for atmospheric research located between the Southern Alps and the northern Mediterranean Sea.
These findings indicate that the hydrologic response of mountain catchments to atmospheric warming and reduced snowfall may substantially vary across elevations with differing soil and regolith properties, a relationship not typically accounted for in approaches relying on space-for-time substitution.
VISITORS TO SICHUAN'S atmospheric mountains, home to both Tibetan and Qiang minorities, used to skip Yingxiu village on their way to more scenic spots higher up.
Casa Il Carmine, Erice At the entrance to the ancient, atmospheric mountain-top town of Erice, the rooms at this converted convent still feel a little like nuns' cells, in a good way – calm and contemplative.
Thus, the goals of this expedition are to collect data that will shed light on the sensitivity of Himalayan mountain glaciers to rising atmospheric temperatures, and to place these glaciers into the context of past climate change.
InSAR can overcome this deficit and can be used as a unique meteorological observation technique to elucidate small-scale spatial structures of mountain waves and other atmospheric phenomena.
The idea is quite old and started with the determination of the thickness of snow layers on a mountain by means of atmospheric muons (George, 1955).
They consist of advection across the poles, steady state geostrophically balanced flow of both global and local scales, forced nonlinear advection of an isolated low, zonal flow impinging on an isolated mountain, Rossby-Haurwitz wands, and observed atmospheric states.
