HYDROMETEROLOGY (LESSON 1..6B)

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WIND AND ITS HYDROLOGIC IMPLICATIONS

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Grace Balahay

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HYDROMETEROLOGY (LESSON 1..6B)


HYDROMETEROLOGY (LESSON 1..6B)Versión en línea WIND AND ITS HYDROLOGIC IMPLICATIONS por Grace Balahay 1 Air in motion Written answer 2 It is a natural phenomenon that is influenced by a variety of factors, including the Earth's rotation, temperature gradients, and the composition and structure of the atmosphere. Written answer 3 from which the wind is blowing Written answer 4 the wind doesn't flow directly from high to low pressure but gets deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. Written answer 5 Winds tend to blow from the cooler bodies of water toward the warmer land Written answer 6 Mountains radiate heat at night, this makes the mountains cool. At this time the valley is relatively warm. As a result, cold and heavy winds blow down the mountain. The wind that blows at night towards the bottom of the valley is known as Written answer 7 During the day the mountains are warmer than the bottom of the valley. This causes high pressure at the bottom of the valley and low pressure at the side of the mountain. For this reason, the wind that blows upwards through the mountain during the day is called Written answer 8 Lower layer of the atmosphere where wind speeds are reduced and direction are deflected because of friction produced by trees, buildings, and other obstacles. Written answer 9 lower part of the atmosphere directly influenced by its contact with a planetary surface. • extends from the ground up to a height where atmospheric properties like temperature, moisture, and wind speed become relatively constant with height. Written answer 10 (0-1 cm), molecular transport, no turbulence Written answer 11 (0-100 m), strong gradients, very vigorous turbelence Written answer 12 (100m -1 km), well-mixed, vigorous turbulence Written answer 13 inversion, intermittent turbulence Written answer 14 refers to a change in wind speed or direction with height in the atmosphere. It can occur either vertically or horizontally Written answer 15 upward energy transport Written answer 16 Strong winds combined with low temperatures can result in lower effective temperatures, known as the Written answer 17 Refers to the change in temperature with respect to the altitude of an air parcel. Usually focuses on the troposphere due to its impact on the weather Written answer 18 Refers to the change in temperature with respect to the altitude of an air parcel without gaining or losing any heat to the environment surrounding the parcel Written answer 19 6.5 °C/km (or K/km) Written answer 20 Unsaturated air parcels cools ~9.8 °C/km (or K/km) Written answer 21 • Saturated air parcels cools ~3-6 °C/km (or K/km) • Occurs when the air parcels reached dewpoint temp. Written answer 22 Equal temperatures are referred to as Written answer 23 is determined by raising or lowering this hypothetical air parcel and comparing its properties to those of the surrounding environment. Written answer 24 If a rising air parcel has a lower temperature than the surrounding environment, the rising parcel is denser, and will tend to sink. In this case, the atmosphere is said to be Written answer 25 If a rising air parcel has a higher temperature than the surrounding environment, the rising parcel is less dense, and will continue to rise. In this case, the atmosphere is said to be Written answer 26 vertical motion is suppressed, and a displaced parcel will move back toward its original position. Written answer 27 air parcels displaced either upward or downward will continue in that direction Written answer

HYDROMETEROLOGY (LESSON 1..6B)

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Creada por

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HYDROMETEROLOGY (LESSON 1..6B)Versión en línea

por Grace Balahay

Air in motion

It is a natural phenomenon that is influenced by a variety of factors, including the Earth's rotation, temperature gradients, and the composition and structure of the atmosphere.

from which the wind is blowing

the wind doesn't flow directly from high to low pressure but gets deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.

Winds tend to blow from the cooler bodies of water toward the warmer land

Mountains radiate heat at night, this makes the mountains cool. At this time the valley is relatively warm. As a result, cold and heavy winds blow down the mountain. The wind that blows at night towards the bottom of the valley is known as

During the day the mountains are warmer than the bottom of the valley. This causes high pressure at the bottom of the valley and low pressure at the side of the mountain. For this reason, the wind that blows upwards through the mountain during the day is called

Lower layer of the atmosphere where wind speeds are reduced and direction are deflected because of friction produced by trees, buildings, and other obstacles.

lower part of the atmosphere directly influenced by its contact with a planetary surface. • extends from the ground up to a height where atmospheric properties like temperature, moisture, and wind speed become relatively constant with height.

(0-1 cm), molecular transport, no turbulence

(0-100 m), strong gradients, very vigorous turbelence

(100m -1 km), well-mixed, vigorous turbulence

inversion, intermittent turbulence

refers to a change in wind speed or direction with height in the atmosphere. It can occur either vertically or horizontally

upward energy transport

Strong winds combined with low temperatures can result in lower effective temperatures, known as the

Refers to the change in temperature with respect to the altitude of an air parcel. Usually focuses on the troposphere due to its impact on the weather

Refers to the change in temperature with respect to the altitude of an air parcel without gaining or losing any heat to the environment surrounding the parcel

6.5 °C/km (or K/km)

Unsaturated air parcels cools ~9.8 °C/km (or K/km)

• Saturated air parcels cools ~3-6 °C/km (or K/km) • Occurs when the air parcels reached dewpoint temp.

Equal temperatures are referred to as

is determined by raising or lowering this hypothetical air parcel and comparing its properties to those of the surrounding environment.

If a rising air parcel has a lower temperature than the surrounding environment, the rising parcel is denser, and will tend to sink. In this case, the atmosphere is said to be

If a rising air parcel has a higher temperature than the surrounding environment, the rising parcel is less dense, and will continue to rise. In this case, the atmosphere is said to be

vertical motion is suppressed, and a displaced parcel will move back toward its original position.

air parcels displaced either upward or downward will continue in that direction