exam 2 Flashcards
what are the three main temperature scales
fahrenheit, celsius, kelvin
who developed the Fahrenheit scale and in what year
Gabriel Daniel Fahrenheit ; 1714
based on mercury-in-glass thermometer based upon a “zero point” ; only in US
Fahrenheit Scale
what are the three significant temperatures on the Fahrenheit scale
98.6 - human body temperature
212 - water’s boiling/steam point
32 - freezing/”zero” point
who developed the Celsius scale and in what year
Anders Celsius ; 1742
devised using the decimal scale and a “zero” point; used widely worldwide (except US)
Celsius Scale
a degree of celsius is ________ (smaller/larger) than a degree of Fahrenheit by a factor of _____
larger ; 1.8
what are the three significant temperatures on the Celsius scale
37 - human body temperature
100 - water’s boiling/steam point
0 - freezing point
who developed the Kelvin scale and in what year
Lord Kelvin (William Thompson) ; 1848
used in scientific formulas/applications ; no negatives on this scale ; the “zero” point is the cessation of molecular motion
Kelvin Scale
what are the significant temperatures on the Kelvin scale
273 - freezing point of water
373 - water’s boiling/steam point
temperature scale conversion: Fahrenheit to Celsius
(F - 32) / 1.8 = C
EX: 50 F = 10 C
(50 F - 32) / 1.8 = 18 / 1.8 = 10C
temperature scale conversion: Celsius to Fahrenheit
C x 1.8 + 32 = F
EX: 30 C = 86 F
(30 C x 1.8) + 32 = 86 F
units of measure ; developed in the early 20th century ; a method of evaluating energy demand and consumption
Heating/Cooling Degree Days
what is the daily mean temperature that marks/determines when to be heating or cooling
65 F / 18.3 C
if the average temperature is >65…
CDD
if the average temperature is
HDD
the degree difference between the average temperature and 65 F tells you…
the number of HDD or CDD
EX: high temp is 90 F , low temp is 60 F ; therefore the average temp is 75 F ; this is 10 F > 65 F ; therefore, it would be a 10 CDD observed for the day
CDD season
Jan - Dec
HDD season
July 1 - June 30
what are the 2 factors of the heat stress index
temperature and humidity
85% of body heat loss is from…
top of head to neck/shoulders
what are the 2 main factors of the wind chill index
air temperature and wind speed
what is the most important compound in the atmosphere
water vapor
the amount of water vapor (gas) in the atmosphere is _____ (higher/lower) in the polar regions and _____ (higher/lower) near the equator/tropical regions
lower (near 0%) ; higher (near 4%)
water vapor is very important when considering…
atmospheric stability
latent heat absorbed…
- *Cooling Process
- evaporation
- melting
- sublimation
> LAMES
latent heat released…
- *Warming Process
- freezing
- condensation
- deposition
> LRCDF
humidity
refers to any one of a number of different ways of specifying the amount of water vapor in the air
(AKA-water vapor density) ; the weight/mass of the water vapor per volume of air parcel
absolute humidity
comparing the weight/mass of the water vapor per volume of air parcel with the total weight/mass of the air in the parcel including the water vapor
specific humidity
comparing the weight/mass of the water vapor per volume of air parcel with the weight/mass of the remaining dry air
mixing ratio
ratio of the air’s actual water vapor content compared with the amount of water vapor required for saturation at a given temp
relative humidity
relative humidity can be influenced, or changed, by…
- adding/subtracting moisture to air
- changing given air temp
relative humidity has _______ relationship to temperature
inverse ; so if temperature is getting higher throughout the day, RH is getting low
the temperature to which a parcel of air would need to be cooled to (assuming no change in air pressure or moisture content) in order for the given parcel of air to reach saturation
dew point temperature
dew point temperature is always __________ air temperature
less than or equal to
when dew point temp = air temp…
air is saturated (relative humidity = 100%)
relative humidity is lowest when…
there is a greater difference between dew point temp and air temp
relative humidity is highest when…
there is a smaller difference between dew point temp and air temp
a lower dew point temperature means…
less moisture in air (cold air can hold less water)
a higher dew point temperature means…
more moisture in air
dew cell
directly measures the air’s actual water vapor pressure (used in ASOS/AWOS sensor systems)
atmospheric stability refers to…
a state of equilibrium of the atmosphere
in order to determine atmospheric stability, we look at…
the temperature of a parcel of air as it rise and/or sinks in the atmosphere and compare that temperature to the temperature of surrounding air
when you force a parcel of air to rise…
it expands and cools
when you force a parcel of air to sink
it compresses and warms
when a given parcel of air expands/cools or compresses/warms with NO interchange of heat with its outside environment
adiabatic process
in unsaturated air, air cools/heats at a rate of…
5.5 F / 1000 Ft
in saturated air, air cools/heats at a rate of…
3.3 F / 1000 Ft
when the ELR is greater than the DALR, the atmosphere is said to be
absolutely unstable
when the ELR is greater than the MALR, but less than the DALR, the atmosphere is said to be
conditionally unstable
when the ELR is less than the MALR, the atmosphere is said to be
absolutely stable
stability is enhanced by…
- radiational cooling of the earth’s surface after sunset
- cooling of air mass from below as it moves over a colder surface
- subsidence of an air column
instability is enhanced by…
- intense solar heating
- heating of air mass from below as moves over a warmer surface
- forceful lifting of air (orographic and frontal)
- upward motion with surface air convergence
- radiational cooling from nocturnal thunderstorm cloudtops
parcels rise in _____ (warmer/colder) air
warmer
ELR
Environmental Lapse Rate ; rate at which air cools with height
water that has condensed onto objects near the ground when the temperature of those objects has cooled below the dew point temperature of the surrounding air ; not a form of precipitation, but still an important source of moisture
dew