Thus our equation predicts S = 0 in a long narrow zone (something similar to an eye) and the existence of a streamline discontinuity (as per hurricane eye) in a narrow
zone near the equator.
These merge and rise in the intertropical convergence
zone near the Equator and blow eastward and poleward at altitudes of 2 to 17 km (1 to 11 miles).
The rising air creates a low pressure
zone near the equator.
Not exact matches
University of Pittsburgh biologists Matthew Koski and Tia - Lynn Ashman recently looked at 34 different populations of silverweed cinquefoil, a widespread plant native in temperate
zones on both sides of the
equator, and found that its flowers were darker
near the tropics.
Powerful eruptions can wreak havoc on monsoons by shifting and weakening the Intertropical Convergence
Zone, a belt of low pressure
near the
equator that drives nearby precipitation patterns.
With temperate -
zone countries seeing possible agricultural benefits through 2050 under the 2007 assessments of the Intergovernmental Panel on Climate Change, even as conditions grow tougher
near the
Equator, how much does self - interest trump broader responsibilities?
Inter-Tropical Convergence
Zone (ITCZ)- The Inter-Tropical Convergence
Zone is an equatorial zonal belt of low pressure
near the
equator where the northeast trade winds meet the southeast trade winds.
The Intertropical Convergence
Zone (ITCZ), is the area encircling the earth
near the
equator where the northeast and southeast trade winds come together.
During periods when the intertropical convergence
zone (ITCZ) is located
near the
Equator, trade winds from the northeast and southeast converge there.
The Intertropical Convergence
Zone (ITCZ), known by sailors as the doldrums, is the area encircling Earth
near the
Equator, where the northeast and southeast trade winds converge.
The narrow
zone of uplift in the tropics produces high, thick clouds in the ITCZ (which is
near the
equator).
Hadley Cell A direct, thermally driven overturning cell in the atmosphere consisting of poleward flow in the upper troposphere, subsiding air into the subtropical anticyclones, return flow as part of the trade winds
near the surface, and with rising air
near the
equator in the so - called Intertropical Convergence
Zone.
These moisture variations result from the movements of the intertropical convergence
zone, a narrow belt of abundant precipitation that encircles Earth
near the
Equator.
Examining the structure of the global cloud field one can see, a long line of bright, dense clouds
near the
equator in a region known as the Intertropical Convergence
Zone (ITCZ), more clearly evident over the tropical Atlantic and East Pacific oceans.
-- Tropical — occur
near the
equator, in low latitudes — Temperate — occur about halfway between the
equator and the poles, in the middle latitudes — Polar — occur
near the poles, in the high latitudes — Dry — occurs at many different latitudes — Highland — occurs at many different latitudes Geographers divide some climate
zones into more specific climate regions.