1. AOSC
Lesson 4

3. Fig. 2-15, p. 43

4. Fig. 2-16, p. 44

5. Table 2-2, p. 44

6. Fig. 2-17, p. 45

7. The Earth’s Orientation
EARTH'S AXIS IS NOT PERPENDICULAR TO THE PLANE OF ITS ORBIT AROUND THE SUN.
IT IS TILTED 23.5 DEGREES FROM THE PERPENDICULAR
INCLINATION OF THE AXIS.
WITHOUT THIS INCLINATION WE WOULD HAVE NO SEASONS.
THIS CHANGES THE SOLAR ZENITH ANGLE OF THE SUN, AND THE AREA COVERED BY A BEAM OF SUNLIGHT
AREA COVERED BY BEAM IS PROPORTIONAL TO 1/COS OF THE SOLAR ZENITH ANGLE
IN COLLEGE PARK, SOLAR ZENITH ANGLE OF THE SUN IS 67 DEGREES ON DEC 22, AND 19 DEGREES ON JUNE 22. THE RATIO OF 1/COS OF THE ANGLES IS ABOUT 2. TWICE AS MUCH ENERGY FALLS ON UNIT AREA AT THE GROUND IN SUMMER THAN IN WINTER.
THE LENGTH OF THE DAY ALSO VARIES WITH SEASON – ALSO A RESULT OF THE INCLINATION OF THE EARTH.

8. Fig. 2-19, p. 49

9. Incoming Solar Radiation
25% PENETRATES DIRECTLY TO EARTH'S SURFACE.
26% SCATTERED BY ATMOSPHERE BUT THEN REACHES THE SURFACE.
TOTAL OF 51% REACHES SURFACE.
31% REFLECTED BACK TO SPACE BY CLOUDS, ATMOSPHERIC SCATTERING, AND REFLECTIVE SURFACES, E.G. SNOW AND ICE.
19% ABSORBED BY CLOUDS AND ATMOSPHERIC GASES

10. Absorption • GASES ARE EXCELLENT ABSORBERS.
WHEN RADIATION IS ABSORBED, ENERGY IS CONVERTED INTO INTERNAL MOLECULAR MOTION - RISE OF TEMPERATURE.
SIGNIFICANT ABSORBERS ARE:
OXYGEN AND OZONE
WATER VAPOR

11. Reflection
THE FRACTION OF ENERGY THAT IS REFLECTED BY A SURFACE IS CALLED ITS ALBEDO.
ALBEDO OF THE EARTH AS A WHOLE IS 30%.
ALBEDO OF FRESH SNOW IS 80-85%
THICK CLOUD - 70 TO 80%
WATER - DEPENDS ON ELEVATION OF THE SUN, FROM 50 TO 80% NEAR HORIZON, 3-5% AT 90 DEGREES.
SOIL- 10%

12. Scattering PRODUCES DIFFUSE LIGHT
SHORTER WAVELENGTHS (BLUE AND VIOLET) ARE SCATTERED MORE EFFECTIVELY THAN LONGER WAVELENGTHS (RED AND ORANGE).
HENCE SKY APPEARS BLUE WHEN VIEWED AT NOON.
AT SUNSET PREFERENTIALLY SCATTERING DEPLETES AMOUNT OF BLUE LIGHT IN DIRECT BEAM - BEAM APPEARS REDDISH.
SCATTERING MORE EFFICIENT AS PARTICLE GETS LARGER - AEROSOLS OR DUST.

14. Fig. 2-20, p. 50

15. Latitudinal Heat Balance
FOR THE GLOBE AS A WHOLE, THE AMOUNT OF INCOMING SOLAR RADIATION IS EQUAL TO THE OUTGOING TERRESTRIAL RADIATION.
HOWEVER THIS STATEMENT DOES NOT HOLD TRUE AT ANY GIVEN LATITUDE
IN GENERAL THERE IS A SURPLUS OF ENERGY AT THE EQUATOR - MORE RADIATION COMES IN THAN GOES OUT
THERE IS ALSO A DEFICIT OF ENERGY AT THE POLES – MORE RADIATION GOES OUT THAN COMES IN.
WHY THEN DO THE POLES NOT GET COLDER AND THE EQUATOR HOTTER?
BECAUSE HEAT IS TRANSPORTED FROM THE EQUATOR TO THE POLES BY OCEAN CURRENTS (E.G. THE GULF STREAM) AND BY THE ATMOSPHERE.

16. Simple Greenhouse Model

17. Fig. 3-2, p. 55

18. Greenhouse Effect

19. Greenhouse Effect

20. Greenhouse Effect