weather and climate change (precipitation) Flashcards

(43 cards)

1
Q

relative humidity

A

60/100 the humidity compared to the total that can be achieved

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2
Q

absolute humidity

A

amount of water vapour present in specific amt of air

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3
Q

relationship of temp and relative humidity

A

temp inc, relative humidity dec (inversely related)

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4
Q

why temp inc, relative humidity dec?

A

temp inc, air expands, total humidity achievable inc, but humidity remains the same, therefore, less relative humidity

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5
Q

saturation

A

relative humidity is 100%

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6
Q

the temperature at which saturation occurs

A

dew point temp

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7
Q

where does dew point temp usually take place?

A

higher in the atmosphere

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8
Q

what areas are very humid?

A

equatorial zone

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9
Q

why is it so humid in the tropics?

A
  1. recieve large amounts of solar radiation which inc the rate of evaporation.
  2. the presence of vegetation increases evapotranspiration and increases humidity too.
  3. nearby oceans and lakes facilitate evaporation.
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10
Q

how to measure humidity

A

dry bulb (dry muslin sleeve)
wet bulb (wet muslin sleeve)

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11
Q

dry bulb

A

atmosphere temp

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12
Q

wet bulb

A

water evaporates bulb cools. produces temp diff between 2 thermometers. amt of evaporation and cooling of the bulb depends on relative humidity.

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13
Q

how to calculate RH with dry and wet bulb

A

use the calculation table to compare dry and wet bulb temperature differences (wet bulb depression)

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14
Q

sling psychrometer procedure

A

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

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15
Q

rationale for ensuring that there ins water in the enclosure sling psychrometer

A

for the wet bulb thermometer to function

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16
Q

rationale for holding the sling psychrometer above your head when swinging

A
  • 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
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17
Q

rationale for swinging sling psychrometer for 1 minute

A

gives sling psychrometer enough time to stabilise reading

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18
Q

reason for repeating sling psychrometer steps

A

more readings to average out inconsistencies, and discrepancies, ensures accuracy

19
Q

weather tracker

A
  • Wind Speed
  • Air/Water/Snow temperature
  • Wind Chill
  • Relative Humidity
  • Heat Stress Index
  • Dewpoint Temp
  • Wet Bulb Temp
  • Barometric Pressure
  • Altitude
  • Density Altitude
20
Q

clouds

A

a visible mass of water droplets or ice crystals that are suspended in the atmosphere

21
Q

cloud formation

A
  1. HEAT causes water to EVAPORATE into WATER VAPOUR
  2. WARM AIR containing water vapour starts to RISE
  3. Air is COOLED RAPIDLY as it rises because TEMPERATURE DECREASES WITH ALTITUDE
  4. 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)
  5. (condensation)
  6. Water droplet condenses on dust particles which act as
    CONDENSATION NUCLEI, tiny water droplets form around
    these particles.
  7. COALESCENCE takes place
22
Q

coalescence

A

Water droplets collide with each other and merge into larger water droplets

23
Q

condensation

A

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

24
Q

okta scale

A

shaded area represents the portion of the sky that is covered by clouds

25
precipitation
water in any form that falls from the atmosphere to the surface of the earth (hail, snow, rain)
26
types of rain
convectional rain relief/orographic rain frontal rain
27
convectional rain process
1. The surface of the earth is HEATED INTENSELY which warms the AIR near the surface 2. The air EXPANDS and RISES as it is heated, its CAPACITY to hold water vapour also INCREASES 3. As warm air rises, it COOLS gradually and can no longer hold as much water vapour, the RELATIVE HUMIDITY of the parcel of air INCREASES 4. At a certain altitude, the relative humidity of the air reaches 100%. CONDENSATION occurs and tiny droplets of water condense around the dust particles in the air 5. Tiny water droplets COALESCENCE to form clouds. High evaporation and rapid condensation result in cumulonimbus clouds to form, leading to convectional rain
28
what is convectional rain usually associated with
convectional rain (thunderstorms) are usually associated with lightning and thunder
29
convectional rainfall intensity
intense: a large amount of water falls as rain over a short period of time
30
relief rain (orographic rain) process
1. A PARCEL OF AIR blows across a WATER BODY and picks up MOISTURE 2. As this parcel of air approaches a mountain, the moist air is forced to RAISE UP THE SLOPE 3. As warm air rises, it COOLS gradually and can no longer hold as much water vapour, the relative humidity of the parcel of air increases 4. At a certain altitude, the relative humidity of the air reaches 100%. CONDENSATION occurs and tiny droplets of water condense around the dust particles in the air 5. Tiny water droplets merge COALESCENCE to form clouds. 6. When the water droplets are heavy enough, they fall as rain on the WINDWARD SIDE
31
windward side
the direction that the wind is blowing
32
what happens to the non-windward side of the mountain
it is DRY. it is called the LEEWARD SIDE or the RAIN SHADOW AREA because the parcel of air decreases in altitude, warms up and can hold more water vapour (relative humidity decreases)
33
how to measure rainfall
rain gauge
34
where to place a rain gauge?
1. On short grass in an open area 2. Far away from buildings and other obstructions. 3. Sunk into the ground with the rim 30 cm above ground 4. NOT on concrete ground
35
why should you place a rain gauge on short grass in an open area?
to prevent water collected on leaves of trees from dripping in
36
why should you place a rain gauge far away from buildings and other obstructions?
to prevent water collected on roofs of buildings from dripping in
37
why should you place a rain gauge sunk into the ground with the rim 30 cm above ground?
to prevent topping over by a human or other living things
38
why can you not place a rain gauge on the concrete ground?
to prevent rainwater from splashing into it from the hard surface of the concrete
39
how to use weather tracker
1. Switch on the weather tracker, switch to the intended mode 2. Hold the weather tracker at one- arm’s length 3. Ensure that the sensor and the fan is not covered 4. For wind speed: Hold weather tracker above head.
40
switch on weather tracker switch to intended mode rationale
Allow for accurate recording of data
41
Hold the weather tracker at one- arm’s length rationale
Prevent the sensors from picking up body heat or moisture
42
Ensure that the sensor and the fan is not covered rationale
Allow for accurate recording of data
43
For wind speed: Hold weather tracker above head rationale
Allow air to flow freely to record accurate wind speed data