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My Meteorology Book _for_blog
My Meteorology Book _for_blog

... 5. Arctic Task 1□ weather Task 2 □ region in US where it is found ...
Climate and Weather
Climate and Weather

... clash with Continental Arctic air masses. ...
Document
Document

... the atmosphere when warm air rises, cools and looses its capacity to hold water vapor. As a result, excess water vapor condenses to form cloud droplets. ...
Mrs. Wisher
Mrs. Wisher

... • Wind is the horizontal movement of air • Winds are caused by the unequal heating of the atmosphere • Winds will travel from an area of high pressure to low pressure • http://hint.fm/wind/ ...
Γ = Γ ∙ (1)
Γ = Γ ∙ (1)

Topic_VI_Meteorology
Topic_VI_Meteorology

... 1. Cold Front: dense cold air forces warm moist air upward creating heavy precipitation for short periods of time at the frontal boundary. ...
Convection Currents and the Mantle
Convection Currents and the Mantle

... As you already know, the earth's mantle contains two layers; the stratosphere (tough liquid part of the outer mantle) and the lithosphere (the stiffer outer mantle and the crust). Because of the intense pressure and temperature in the mantle convection currents occur. To learn about what influence t ...
Global Winds: Warm Low Pressure Air
Global Winds: Warm Low Pressure Air

... MOONSOON RAINS are seasonal and experienced in India & S.E. Asia (subtropical locations) Summer – Land in warmer (Low Pressure) than Water (High Pressure). Air moves from water to land carrying moisture --- RAIN. It can rain 37 ft of rain in a few months. Remember … Land heats up faster than water. ...
chapter 5 energy, matter, and momentum exchanges near the surface
chapter 5 energy, matter, and momentum exchanges near the surface

... atmosphere to rise or sink spontaneously o In a stable atmosphere, if a parcel is forced to rise for any reason, it will sink once the lifting force is removed, because it is cooler than the air adjacent to it at a given level o Positive buoyancy, which occurs in an unstable atmosphere, refers to a ...
Thermal Convection vs. Thermal Conduction
Thermal Convection vs. Thermal Conduction

Global Climates and biomes
Global Climates and biomes

AIM: OBJ: DN: HW:
AIM: OBJ: DN: HW:

Transfer of Thermal Energy worksheet
Transfer of Thermal Energy worksheet

... Conduction is the transfer of heat energy from one substance to another or within a substance. Have you ever left a metal spoon in a pot of soup being heated on a stove? After a short time the handle of the spoon will become hot. This is due to transfer of heat energy from molecule to molecule or fr ...
The Difference Between Weather and Climate
The Difference Between Weather and Climate

... Air Pressure: the weight of air pushing on Earth’s surface Humidity: the amount of water vapor in the air Drought: a long period of very low rainfall; may last up to several years *** A drought can be very dangerous to people, animals, and plants, since we all need water to survive. ...
Chapter 1 - Weather Underground
Chapter 1 - Weather Underground

Science Chap 7,8,9 study guide
Science Chap 7,8,9 study guide

... 8. A band of very fast wind that is formed by the different temperatures between huge convection currents is called a __________ ____________________. 9. When rocks are squeezed and heated at very high temperatures, they can be changed into ____________________ rock. 10. The top part of Earth’s ____ ...
Lecture Packet#1
Lecture Packet#1

... an average rate of 3.5° F per thousand feet (6.5 ° C per kilometer); whereas the stratosphere has either constant or slowly increasing temperature with height. The troposphere is where all of Earth's weather occurs. The boundary that divides the troposphere from the stratosphere is called the "tropo ...
What is Weather.
What is Weather.

...  Others … He, H, neon, ozone and krypton.  This air thins out quickly as you increase altitude.  Air always contains some water vapor. Humidity. ...
Weather Forecasting
Weather Forecasting

... Warm Front What type of weather does this front bring? ...
Worksheet 2
Worksheet 2

Introduction To Weather Dynamics
Introduction To Weather Dynamics

... •Explain how areas of high and low pressure move air and energy around the globe ...
Chapter 13: The Atmosphere Learning Target Vocabulary Word
Chapter 13: The Atmosphere Learning Target Vocabulary Word

... Heat is transferred in three ways: ______________, ______________and ______________. Heat is transferred mostly by convection within the ______________. ...
Maritime equatorial (mE)
Maritime equatorial (mE)

... Denser, advancing cold air forces warm, moist air to lift abruptly. As the air is lifted, it cools by expansion, cooling to the dew - point as it rises it condenses and forms clouds. Cumulonimbus clouds may produce large raindrops, heavy showers, lightning and thunder, and hail. ...
POWERPOINT SCIENCE
POWERPOINT SCIENCE

... temperature to a region of lower temperature, and acts to equalize temperature differences. It is also described as heat energy transferred from one material to another by direct contact. ...
Lightning
Lightning

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Atmospheric convection



Atmospheric convection is the result of a parcel-environment instability, or temperature difference, layer in the atmosphere. Different lapse rates within dry and moist air lead to instability. Mixing of air during the day which expands the height of the planetary boundary layer leads to increased winds, cumulus cloud development, and decreased surface dew points. Moist convection leads to thunderstorm development, which is often responsible for severe weather throughout the world. Special threats from thunderstorms include hail, downbursts, and tornadoes.
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