kinetic energy in the atmosphere kinetic energy is the energy of motion heat - the total kinetic...
DESCRIPTION
Methods of Heat Flow Conduction - heat transfer through collisions between neighboring atoms; requires direct contact Solids are better conductors of heat energy than liquids Liquids are better conductors of heat energy than gasesTRANSCRIPT
![Page 1: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/1.jpg)
Kinetic Energy In The Atmosphere• Kinetic Energy is the energy of motion• Heat - the total kinetic energy of the
atoms composing a substance (atmospheric components)• Temperature - a measure of the average
kinetic energy of the atoms• Scales:− Fahrenheit−Celsius−Kelvin
![Page 2: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/2.jpg)
Transport of Heat Energy • A Temperature Gradient shows the
change in temperature over distance
• Heat flows from locations of higher temperatures toward locations of lower temperatures (2nd Law of Thermodynamics)
![Page 3: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/3.jpg)
Methods of Heat Flow •Conduction - heat transfer through collisions between neighboring atoms; requires direct contact• Solids are better conductors of heat
energy than liquids• Liquids are better conductors of heat
energy than gases
![Page 4: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/4.jpg)
•Convection - heat transfer within a fluid (liquids & gases)
• Warm fluids are less dense than cold fluids
• Denser fluids descend & push warmer, less dense fluids upward
• Is the main method of transferring heat vertically in the troposphere
• Sensible heating - the combined processes of conduction and convection
![Page 5: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/5.jpg)
•Radiation - the transfer of heat energy through electromagnetic waves
• Is the primary method of atmospheric heating from the sun
• Is primary method of heat escape into space• Energy can travel through vacuum
![Page 6: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/6.jpg)
Heat Imbalance vs. Equilibrium • Heat Imbalance refers to the variations
in radiational heating and cooling throughout the Earth’s atmosphere
• Result of heat imbalance is temperature gradients
• Although there are variations of heat energy within the atmosphere, Earth is in radiational equilibrium
![Page 7: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/7.jpg)
Heat Imbalance & Latitude • Incoming solar radiation strikes lower
latitudes more directly than higher latitudes
• High latitudes have lower solar intensity• Latitudes poleward of 30 degrees North
or South experience net cooling• Latitudes within 30 degrees of the
equator experience net heating
![Page 8: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/8.jpg)
• Heat is transported from lower latitudes to higher latitudes by way of three mechanisms:• Air mass exchange
− Types of air masses (based on their origin)− Cold / Humid− Cold / Dry− Warm / Humid− Warm / Dry
![Page 9: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/9.jpg)
•Storms−At lower latitudes, water evaporates
from surface water and is drawn into storm circulation−As storm travels to higher latitudes,
water vapor condenses to form clouds and precipitation, releasing latent heat into the atmosphere
![Page 10: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/10.jpg)
•Ocean Circulation−Water currents carry warm water at
lower latitudes toward higher latitudes−Example - Gulf Stream
![Page 11: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/11.jpg)
Latent Heating • Equilibrium within the atmosphere is
maintained through latent heating.• Latent Heating is the transfer of heat
energy from place to place as a consequence of changes in the phase of water• During phase changes, heat energy is either
absorbed or released• Condensation & freezing release latent heat
into the environment• Melting & evaporation absorb heat from the
environment
![Page 12: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/12.jpg)
Specific Heat • Specific Heat is the amount of heat
required to change the temperature of one gram of a substance 1 degree Celsius• A substance with low specific heat warms
up more than a substance with a higher specific heat
• Water has the greatest specific heat of all natural substances
![Page 13: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/13.jpg)
•Specific heat differences is the main reason land surface temperatures vary more than lakes & oceans• Land heats up more during day/summer
and cools down more at night/winter• Water has greater resistance to
temperature change - Thermal Inertia• Locations close to large bodies of water
exhibit smaller seasonal temperature variations than inland locations
![Page 14: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/14.jpg)
Temperature Related Indexes
•Heating & Cooling Degree Days•Heating Degree Days are a measure of the number of days needed to heat buildings
• Cooling Degree Days are a measure of the number of days needed to cool buildings
• The daily average temperature is compared to 65F• Temp. averages less than 65F require heating• Temp. averages greater than 65F require cooling
![Page 15: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/15.jpg)
•Windchill Equivalent Temperature (WET)
• A temperature determination due to the combined effects of cold temperature and wind speed
• A layer of still air surrounds the skin due to heat being conducted from the skin to the cold air (temperature gradient) - Boundary layer
• Air is a poor conductor of heat; thus the boundary layer helps insulate the body from heat loss
![Page 16: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/16.jpg)
• As wind speed increases, the boundary layer thickness diminishes
• The body experiences an increase in heat loss
• Wind speeds greater than 35 mph have minimal increased effect
![Page 17: Kinetic Energy In The Atmosphere Kinetic Energy is the energy of motion Heat - the total kinetic energy of the atoms composing a substance (atmospheric](https://reader036.vdocuments.us/reader036/viewer/2022082501/5a4d1b167f8b9ab0599917b1/html5/thumbnails/17.jpg)
•Heat Index (Apparent Temperature)
• A combination of temperature and humidity influence the rate of surface skin water evaporation
• Higher humidity reduces the evaporative process; surface skin temperature increases
• Other factors influencing apparent temperature include:
• Cloud cover• Air pressure• Wind speed