Air temperature controls
Frost, Dew, Fog
Atmospheric Stability
Humidity
Biometerological Applications
100

Formula to convert C to F

What is (C*1.8)+32

100

A byproduct of deposition when you cool the temperature of an object below the dew point temp of the surrounding air and the air temperature is below freezing 

What is frost 

100

Colder air aloft- parcels move (faster or slower), (instability or stability)

faster, instability 

100
Dew point temperature and air temperature close together (with respect to relative humidity) 

What is a higher relative humidity 

100

Absorbed heat becomes latent heat when being absorbed 

What is evaporation

200

The four air temperature controls from place to place

What are differential heating of land and water, ocean current temperatures, elevation and latitude/geographic position (exposure)

200

A byproduct of condensation when you cool the temperature of an object below the dew point temperature of the surrounding air and the air temperature is above freezing

What is dew 

200

Solar heating, horizontal (colder to warmer) heating of airmass as it moves over a warmer surface, dynamic lifting of air, surface convergence air, radiative cloud top cooling from thunderstorms in adjacent areas

What enhances unstable air 

200

Comparing the weight/mass of water vapor volume per parcel of air to the dry air in the parcel 

What is the mixing ratio

200

2 PART 

If the relative humidity is higher and the air temperature is warmer, sweat occurs (faster or slower) with (more or less energy)

What is slower, more (think steam not sauna)

300
The Heating Degree Day Season

When is July 1-June 30

300

Condensation nucluei (and condensation) + saturation/100% relative humidity= this 

What are clouds 

300

2 PART 

When the 3.3 < ELR < 5.5, same scenario but with unsaturated air 

What is conditionally unstable , absolutely stable 

300

As air temperature increases, relative humidity does this (assuming moisture levels are the same)

What is increases (inverse relationship between air temperature and relative humidity)

300

Biometerological application based on air temperature and wind speed 

What is the wind chill index 

400

The type of degree day (HDD or CDD) when the air temperature is above 65 degrees

What is a cooling degree day 

400

Cooling fog where rising water vapor+ cool air condenses/rises with the air being warmed below. Most common in lakes/barton springs 

What is steam/evaporation fog 

400

Air temp- 3.3 degrees F, used in clouds 

What is the Moist Adiabatic Lapse Rate (MALR)

400

A ratio of the air's actual water vapor/moisture content compared to the amount of water vapor required for saturation at a given temperature. Tells only how close we are to saturation. 

What is relative humidity

400

A more realistic biometerological application based on air temp, relative humidity, sun/solar heating and wind speed 

What is a wet bulb globe temperature 

500

In Austin, which (heating or cooling) requires more energy/is more unpredictable 

What is heating/HDD

500

Ocean fog near the shore/moving inland. In the morning, on the shore, the clouds are over the ocean and land is warming. At night the clouds are over the city and the land is cooling. Most common on west coast. Warm moist air is being blown over a cold surface.

What is advection (cooling) fog 

500

Comparing the temperature of a parcel of air as it rises and falls in the atmosphere to the environmental air temperature 

What is atmospheric stability 

500

The location of the air parcel when there is the dew point is lowest 

What is to the left 

500

Biometerological application based on air temperature and amount of moisture and is a cumulative process

What is the heat stress index