weather and climate change (precipitation) Flashcards
(43 cards)
relative humidity
60/100 the humidity compared to the total that can be achieved
absolute humidity
amount of water vapour present in specific amt of air
relationship of temp and relative humidity
temp inc, relative humidity dec (inversely related)
why temp inc, relative humidity dec?
temp inc, air expands, total humidity achievable inc, but humidity remains the same, therefore, less relative humidity
saturation
relative humidity is 100%
the temperature at which saturation occurs
dew point temp
where does dew point temp usually take place?
higher in the atmosphere
what areas are very humid?
equatorial zone
why is it so humid in the tropics?
- recieve large amounts of solar radiation which inc the rate of evaporation.
- the presence of vegetation increases evapotranspiration and increases humidity too.
- nearby oceans and lakes facilitate evaporation.
how to measure humidity
dry bulb (dry muslin sleeve)
wet bulb (wet muslin sleeve)
dry bulb
atmosphere temp
wet bulb
water evaporates bulb cools. produces temp diff between 2 thermometers. amt of evaporation and cooling of the bulb depends on relative humidity.
how to calculate RH with dry and wet bulb
use the calculation table to compare dry and wet bulb temperature differences (wet bulb depression)
sling psychrometer procedure
1 Ensure that there is water in the enclosure
2 Hold the Sling psychrometer above your head when swinging
3 Swing it for 1 minute
4 Read and record the temperature on the two thermometers (Wet and Dry)
5 Repeat steps 1 to 4
6 Calculate the difference between wet and dry bulb
7 Refer to the conversion table to read R.H
rationale for ensuring that there ins water in the enclosure sling psychrometer
for the wet bulb thermometer to function
rationale for holding the sling psychrometer above your head when swinging
- So that it is far from your body and does not pick up body heat that affects reading
- Safety reasons for not hitting your friend
rationale for swinging sling psychrometer for 1 minute
gives sling psychrometer enough time to stabilise reading
reason for repeating sling psychrometer steps
more readings to average out inconsistencies, and discrepancies, ensures accuracy
weather tracker
- Wind Speed
- Air/Water/Snow temperature
- Wind Chill
- Relative Humidity
- Heat Stress Index
- Dewpoint Temp
- Wet Bulb Temp
- Barometric Pressure
- Altitude
- Density Altitude
clouds
a visible mass of water droplets or ice crystals that are suspended in the atmosphere
cloud formation
- HEAT causes water to EVAPORATE into WATER VAPOUR
- WARM AIR containing water vapour starts to RISE
- Air is COOLED RAPIDLY as it rises because TEMPERATURE DECREASES WITH ALTITUDE
- As the parcel of air rises in the atmosphere, the TEMPERATURE FALS AND RELATIVE HUMIDITY RISES (cool air holds less water vapour compared to warm air)
- (condensation)
- Water droplet condenses on dust particles which act as
CONDENSATION NUCLEI, tiny water droplets form around
these particles. - COALESCENCE takes place
coalescence
Water droplets collide with each other and merge into larger water droplets
condensation
When relative humidity reaches 100% at HIGH ALTITUDES,
the air becomes SATURATED and the excess water vapour
ceases to exist as gas and changes back to water
okta scale
shaded area represents the portion of the sky that is covered by clouds