Title: ATM OCN 100
1ATM OCN 100 Summer 2002 LECTURE 7
- ATMOSPHERIC ENERGETICS RADIATION (cont.)
- A. Introduction
- B. Radiant Energy - Fundamentals
2Announcements
- Homework 1
- Please Pick up yours in front.
- Homework 2
- Get from our webpage
- http//www.aos.wisc.edu/hopkins/aos100/homework/
- Due Monday 1 Oct 2001
3MADISONS CURRENT WEATHER
at 900 AM CDT WED SEP 26 2001 Updated twice an
hour at 05 and 25 Sky/Weather FAIR
Temperature 51 F (10 C) Dew Point 38 F (3
C) Relative Humidity 60 Wind NW10 MPH
Barometer 30.04F
4Rules of Thumb
- Other things being equal
- Cloudy nights have higher temperatures than clear
nights. - Cloudy days have lower temperatures than clear
days.
5(No Transcript)
6This mornings low temperatures (oF)
7This Mornings Low Temperatures (oF) (1961-90)
Average Low Temperatures
8Current Surface Weather Map with Isobars (iso
equal bar weight), Fronts and Radar
9Tomorrow AMs Forecast
10Yesterdays high temperatures (oF)
11Yesterdays High Temperatures (oF) (1961-90)
Average High Temperatures
12Surface Weather Map from Today with Isobars
Fronts
13Current Temperatures (F) Isotherms
14Landsat-7 Image of NW Wisconsin nr Siren 18 May
2001 (Pre tornado)http//www.news.wisc.edu/newsph
otos/siren.html
15Landsat-7 Image of NW Wisconsin nr Siren 19 June
2001 (After tornado)http//www.news.wisc.edu/news
photos/siren.html
16(No Transcript)
17(No Transcript)
18Surface Weather Map from Today with Isobars
Fronts
19Current Temperatures (oF) Isotherms
20Hurricanes Isaac Joyce
21Yesterdays High Temperatures (oF) (1961-90)
Average High Temperatures
22Tomorrows 7AM Forecast
23Current Wind-Chill Equivalent Temperatures (oF)
24ATM OCN 100 - Summer 2002 LECTURE 7
- ATMOSPHERIC ENERGETICS RADIATION
- A. INTRODUCTION
- What is radiation?
- What is significance of radiation?
25B. RADIANT ENERGY orELECTROMAGNETIC RADIATION
- The nature of electromagnetic radiation
- Wave forms
- Terminology describing waves
- Speed of wave
- Wavelength Fig 2.2 Moran Morgan (1997)
- Frequency
26WAVE TERMINOLOGY
- Speed of wave
- miles per hour or meters per second
- Wavelength
- meters or micrometers
- Frequency
- Cycles per second or Hertz
27WAVE TERMINOLOGY (cont.)
- Fundamental Relationship
- Speed wavelength x frequency
28ELECTROMAGNETIC RADIATION FUNDAMENTALS (cont.)
- The Electromagnetic Spectrum
- The entire spectrum
- Typical names
- X-Rays through Radio Waves
- Spectral regions important to meteorology
- UV, Visible, IR (also microwave)
29The Electromagnetic SpectrumSee Fig. 2.1 Moran
Morgan (1997)
ROY G BIV
30The Hazards of UV Radiation
- Region of concern
- UVA
- UVB
- Consequences of increased UV Radiation
- Skin Cancer
- Cataracts
- Changes in Genetic Pool
- The UV Index
31(No Transcript)
32The UV Index (UVI)
- Numerical Values
- Related to time needed to receive sunburn
- UVI 0-2 (Minimal) ? 60 minutes
- UVI gt 10 (Very High) lt 10 minutes
- UVI Values depend upon
- Latitude
- Elevation
- Clouds
- UVI forecasts produced daily by NWS
33(No Transcript)
34Current UVI Forecast
35A June UVI Forecast
36ELECTROMAGNETIC RADIATION FUNDAMENTALS (cont.)
- Important relationships of radiation
- Ideal radiators/absorbers (black bodies)
- The ideal radiator curve
- Total amount of Energy emitted/absorbed
- Region of maximum radiation
where ...
37Electromagnetic Radiation Emission/Absorption as
a function of Temperature
38ELECTROMAGNETIC RADIATION FUNDAMENTALS (cont.)
- Total energy emitted/absorbed.
- (also known as Stefan-Boltzmanns Law)
39ELECTROMAGNETIC RADIATION FUNDAMENTALS (cont.)
- Region of maximum radiation.
- (also known as Wien's Displacement Law)
40ELECTROMAGNETIC RADIATION FUNDAMENTALS (cont.)
- Inverse Square Relationship
- Intensity of incident radiation varies inversely
with square of distance from radiation source
41ELECTROMAGNETIC RADIATION FUNDAMENTALS (cont.)
- Inverse Square Relationship
- Intensity of incident radiation varies inversely
with square of distance from radiation source
42INVERSE SQUARE LAW (cont.)
43INVERSE SQUARE LAW (cont.)
Earth
44ELECTROMAGNETIC RADIATION FUNDAMENTALS (cont.)
- Zenith Angle Relationship
- Intensity of incoming radiation is
- greatest for vertically oriented rays
- least for rays that parallel horizontal surface.
- Intensity of incoming radiation is proportional
to cosine of incident angle (defined as
zenith angle)
45COSINE ANGLE RELATIONSHIP (cont.)
46Solar Altitude Angles at Different LatitudesFig.
2.6 Moran and Morgan (1997)
47C. THE EARTH, THE SUN andTHE RADIATION LINK
- The Sun Solar radiation
- A star with surface temperature ? 6000 K
- Peak radiation ???????m.
48Our Sun Space Environment Center
49Our Sun from Yesterday Space Environment Center
H-Alpha Image
Helium Image
50Sunspot NumbersFig 20.5 Moran Morgan (1997)
51Extra-atmospheric Solar Radiation See Fig 2.3,
Moran Morgan (1997)
52C. THE EARTH, THE SUN THE RADIATION LINK
(cont.)
- Receipt of solar radiation by Earth-atmosphere
system - Solar Constant Incoming solar radiation received
on surface that is - Perpendicular to suns rays
- Above atmosphere
- at mean earth-sun distance.
- Currently accepted value
- 2 cal/cm2/min 1370 Watt/m2.
53INVERSE SQUARE LAW (cont.)
Earth
54C. THE EARTH, THE SUN THE RADIATION LINK
(cont.)
- Our place in the Sun -- Annual diurnal
motions of Earth - Solstices equinoxes
- Local noon sunrise/sunset
55Earths Orbit of Sun The Cause of the Seasons
See Fig. 2.10 Moran Morgan (1997)
56Earths Orbit of Sun The Cause of the Seasons
See Fig. 2.10 Moran Morgan (1997)
57DAYLIGHT-NIGHT (23 JUN)
58DAYLIGHT-NIGHT (21 SEP)
59DAYLIGHT-NIGHT (22 DEC)
60Latitudinal Dependency
61Solar Altitude Angles at Different LatitudesFig.
2.6 Moran and Morgan (1997)
62Our Tilted Earth
63Sun Paths for Mid LatitudesFig. 2.14 Moran and
Morgan (1997)
64Diurnal Variation in Solar Altitude Angle at
Madison
65C. THE EARTH, THE SUN THE RADIATION LINK
(cont.)
- Disposition of solar radiation in
Earth-atmosphere system - Reflected
- Scattered
- Absorbed
- Transmitted
- Albedo
- where...
66ALBEDO
- The reflectivity of a surface
- Albedo of surfaces
- Implications
67C. THE EARTH, THE SUN THE RADIATION LINK
(cont.)
- Terrestrial radiation
- Emitted from earth-atmosphere system
- Radiating temperature ????????
- Peak radiation region ??????m.
68Terrestrial or Long Wave Radiation Emitted at 300
KSee Fig 2.4, Moran Morgan (1997)