| 31. | Throughout this evolution, retrogression of the large-scale atmospheric circulation features is observed in the eastern Pacific North American sector.
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| 32. | The lake level change is strongly modulated by the Pacific Ocean through atmospheric circulations that fluctuate at low frequency.
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| 33. | A slight change in the temperature differential from cloud bottom to top might generate rapid, large-scale changes in atmospheric circulation.
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| 34. | The Earth's atmospheric circulation varies from year to year, but the large scale structure of its circulation remains fairly constant.
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| 35. | Storms in this region can last for several days or more and are often accompanied by persistent atmospheric circulation features.
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| 36. | When atmospheric circulation settles into a characteristic pattern of no rain and high heat over the region, the vegetation dies.
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| 37. | The atmospheric circulation is controlled by the two semi permanent South Atlantic and South Pacific highs, and the Chaco Low.
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| 38. | This lifetime is short enough for the atmospheric circulation to yield the observed uneven distribution of methane across the planet.
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| 39. | The reasons for this latitude and seasonal dependence are complicated, which involve in atmospheric circulation patterns as well as solar intensity.
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| 40. | Walsh believes a shift in atmospheric circulation in the mid-1970s, which brought more warm air to Alaska, enhanced the greenhouse effect.
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