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Byrne, Michael P.; Pendergrass, Angeline G.; Rapp, Anita D.; Wodzicki, Kyle R. (2018). "Response of the
Intertropical Convergence Zone to Climate Change: Location, Width, and Strength".
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shifts corresponding to the seasons. Due to the position of the Sun, the sea surface temperature near the equator (30°S to 30°N), during an
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Convergence zones also occur at a smaller scale. Convergence lines form rows of showers or thunderstorms over a more local area.
196:, drawing in the cooler, dry air from high pressure areas (divergence zones), creating a convection cell commonly known as the
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Schneider, Tapio; Bischoff, Tobias; Haug, Gerald H. (2014). "Migrations and dynamics of the
Intertropical Convergence Zone."
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can trigger development of a convergence line. The heavy rain caused in a short period of time can cause severe flooding.
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Waliser, D.E.; Jiang, X. (2015). "Tropical
Meteorology and Climate: Intertropical Convergence Zone".
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The ITCZ shifts with the tilt of the earth, coinciding with the changing of seasons.
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is directly related to the position of the Sun or the location of the "
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103:. The large-scale convergence zone formed over the equator, the
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Krishnamurti, T.N.; Stefanov, Lydia; Misra, Vasubanhu (2013).
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410:. New York, New York: Springer Science & Business Media.
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Reference Module in Earth
Systems and Environmental Sciences
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and southeasterly trade winds converging in an area of high
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which can be generated when south-westerly winds blow over
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flows meet and interact, usually resulting in distinctive
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is shifted north, following the position of the Sun. The
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The inverse of convergence is divergence, such as the
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converge from both coasts to form lines of cumulus.
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330:"Meteorology Basics: Convergence and Divergence"
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137:An example of a convergence zone is the
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408:Tropical Meteorology: An Introduction
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396:10.1016/B978-0-12-382225-3.00417-5
83:. Large-scale convergence, called
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87:convergence, is associated with
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355:Current Climate Change Reports
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178:Intertropical Convergence Zone
157:that extends from the western
155:South Pacific convergence zone
139:Intertropical Convergence Zone
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105:Intertropical Convergence Zone
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1:
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328:LEUNG Wai-hung (June 2010).
264:region in the U.S. state of
258:Puget Sound Convergence Zone
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7:
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423:10.1007/978-1-4614-7409-8
366:10.1007/s40641-018-0110-5
278:Elsinore Convergence Zone
270:Mohawk–Hudson convergence
153:. Another example is the
18:Convergence (meteorology)
27:Region in the atmosphere
204:Sea surface temperature
256:Some examples are the
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334:Hong Kong Observatory
306:Flooding in Boscastle
298:Pembrokeshire Dangler
280:in the U.S. state of
272:in the U.S. state of
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260:which occurs in the
30:For other uses, see
446:10.1038/nature13636
224:Northern Hemisphere
210:equator," thus the
63:is a region in the
491:Gliding technology
286:Brown Willy effect
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145:which girdles the
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111:to large areas of
97:low-pressure areas
93:baroclinic troughs
73:weather conditions
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416:978-1-4614-7409-8
143:low pressure area
16:(Redirected from
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190:low pressure
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360:: 355-370.
290:Bodmin Moor
262:Puget Sound
248:Sea breezes
208:energy flux
198:Hadley Cell
186:latent heat
182:trade winds
126:Large scale
61:meteorology
45:sea breezes
32:Convergence
486:Atmosphere
480:Categories
312:References
296:; and the
282:California
266:Washington
141:(ITCZ), a
69:prevailing
67:where two
65:atmosphere
440:: 45–53.
302:Irish Sea
251:colliding
242:Mesoscale
42:Mesoscale
294:Cornwall
274:New York
101:cyclones
91:such as
222:in the
216:equinox
161:toward
151:Equator
149:at the
435:Nature
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284:; the
276:; the
194:vacuum
99:, and
77:clouds
147:Earth
412:ISBN
341:2015
232:ITCZ
228:ITCZ
212:ITCZ
188:and
176:The
79:and
49:Cuba
442:doi
438:513
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