Download presentation
Presentation is loading. Please wait.
1
Unit 4 Weather about Doppler Radar
2
weather basics the uneven heating of the Earth’s surface
Where does the energy for weather originate? the uneven heating of the Earth’s surface
5
Heat Transfer in 3 ways:
6
In the US, the general direction that weather systems
weather basics In the US, the general direction that weather systems move is toward the North and East FROM the SW
7
RUNOFF INFILTRATION PRECIPITATION CONDENSATION EVAPORATION ABSORPTION
TRANSPIRATION RUNOFF ABSORPTION INFILTRATION
8
dewpoint are measured in
Station Models Please go to page 13 of the ESRTs Temperature and dewpoint are measured in degrees _______ 0F
9
.. 76 138 -30\ 55 Cloud Cover Temperature Wind Direction & Speed
Present Weather 55 Dewpoint Barometric Trend Barometric Pressure
11
Barometric Pressure 138 ADD a 9 if the number is above “500” or a 10 if the number is below “500” in front to fit on the scale (ranges from to ) 10138 Add a decimal between the last two digits mb
12
Trend (last 3 hours) The decimal has been omitted (left out) 30 = 3.0
+ means rising - means falling
13
Present weather is light rain
Station models info. Temp Dew cloud Press (mb) Trend Wind Speed 760 F 550 F 100% 1013.8 Falling 3.0 mb NE 15 knots Present weather is light rain
14
Station Model Practice
Wkst 1 and 2
15
MOISTURE page 5
16
Evaporation Rates a- Temperature c- Relative Humidity b- Surface Area
17
as temperature increases, the rate of evaporation
Direct Relationship as temperature increases, the rate of evaporation increases
18
as surface area increases, the rate of evaporation
Direct Relationship as surface area increases, the rate of evaporation increases
19
as the air becomes more saturated, the rate of evaporation
Relative Humidity The % of moisture in the air Inverse Relationship as the air becomes more saturated, the rate of evaporation decreases
20
What natural process cleans the atmosphere? Rain precipitation Snow Hail
21
Cloud Formation
22
dewpoint = condensation
Cools to the dewpoint = condensation Expands & cools Warm Air Rises
23
Clouds are likely to form when:
The air is SATURATED and RISING The temperature is at the DEWPOINT Condensation NUCLEI are available
26
As air temperature increases
the air can "hold" more water
27
lower due to evaporation
Sling Psychrometer Dry bulb measures air temperature Wet bulb temp is lower due to evaporation
28
Using the charts on page 12 of the ESRTs, calculate the relative
humidity and dew point using the following information. Dry Bulb Wet Bulb Difference Dew Point Relative Humidity (%) 14 10 4 20 5 30 19 18 56 6 60 15 12 58 23 7 55 13 5 9 Dewpoint Chart RH Chart
29
Relative Humidity vs Air Temperature
Inverse Relationship as temp. decreases RH increases
30
As dew point increases, the amount of moisture in the air
31
dewpoint get closer together, the probability of precipitation
As temperature and dewpoint get closer together, the probability of precipitation INCREASES
32
Circle the precip. probability
33
probability of precipitation?
Which has the greatest probability of precipitation?
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.