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Climate
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New York State Earth Science June 2007 - Question 03 |
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Saturday, 01 August 2009 09:19 |
Correct Answer: Option 2 – Location A is cooler and wetter than location B
B is in the direction downwind from the point of reference side of the mountain where drier air sinks compresses and warms up creating desert-like regions.
Hence, options 1, 3 and 4 are incorrect.
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Last Updated on Monday, 03 August 2009 09:51 |
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New York State Earth Science June 2007 - Question 27 |
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Saturday, 01 August 2009 09:22 |
Correct Answer: Option 3
In the southern hemisphere the average monthly temperatures slowly start decreasing from January and reach the lowest in the month of July. Later they start rising. Hence, graph in option 3 is the correct representation of the average monthly temperatures in the southern hemisphere. Hence, the options 1, 2 and 4 are incorrect.
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New York State Earth Science June 2007 - Question 46 |
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Saturday, 01 August 2009 09:24 |

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Correct Answer: Option 2 – Prevailing southwesterlies
The planetary atmospheric circulation brings a great variety of air masses to New York State. Masses of cold, dry air frequently arrive from the northern interior of the continent. Prevailing winds from the south and southwest transport warm, humid air, which has been conditioned by the Gulf of Mexico and adjacent subtropical waters. These two air masses provide the dominant continental characteristics of the climate. The third great air mass flows inland from the North Atlantic Ocean and produces cool, cloudy, and damp weather conditions. This maritime influence is important to New York's climatic regime, especially in the southeastern portion of the state, but it is secondary to that of the more prevalent air mass flow from the continent.
Nearly all storm and frontal systems moving eastward across the continent pass through or in close proximity to New York State. Storm systems often move northward along the Atlantic coast and have an important influence on the weather and climate of Long Island and the lower Hudson Valley. Frequently, areas deep in the interior of the state feel the effects of such coastal storms.
Lengthy periods of either abnormally cold or warm weather result from the movement of great high pressure (anticyclonic) systems into and through the eastern United States. Cold winter temperatures prevail over New York whenever Arctic air masses, under high barometric pressure, flow southward from central Canada or from Hudson Bay. High-pressure systems often move just off the Atlantic coast, become more or less stagnant for several days, and then a persistent airflow from the southwest or south affects the state. This circulation brings the very warm, often humid weather of the summer season and the mild, more pleasant temperatures during the fall, winter, and spring seasons
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Last Updated on Saturday, 08 August 2009 09:34 |
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New York State Earth Science June 2007 - Question 47 |
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Saturday, 01 August 2009 09:27 |
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Correct Answer: Option 3 – Warm and wet
The trade winds are the prevailing pattern of easterly surface winds found in the tropics near the Earth's equator. They converge where the climate is warm and wet.
Hence, options 1, 2 and 4 are incorrect.
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Last Updated on Saturday, 15 August 2009 09:08 |
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