Marine Science Laboratory Solar Radiation Revised on 4/24/2007 Page 1 of 9 Name ________________________Lab Section _____________Date _____________. Grade 10/10 MS20 Laboratory: Solar Radiation and Light Transmission Record all data using appropriate metric units (centimeters, grams, etc.). Remember to use significant figure rules and to indicate appropriate units (if the scale reads 13.4 g, your answer is not 13.4, but 13.4 g (or 13.4 grams). A. Measuring a “solar constant” Your numbers will differ because light sources and light meters vary. However, your numbers may be used compare trends shown here. Table one: Distance from light source Measured Light intensity Theoretical (equation 1) 50 cm 500 lux 488 lux 100 cm 122 lux -Æ 122 lux 150 cm 60 lux 54.2 lux 200 cm 34 lux 30.5 Are your measured values of light intensity similar to your calculated (theoretical) values? List several possible sources of error. Meter not held at proper distance or angle. Stray light in the room. Batteries weak, light source inconsistent etc. Earth’s solar constant is 1366 W/m2 (watts per square meter). The planet Venus is 72% of the distance from the Earth to the sun, and the planet Mars is 152%. Ignoring clouds and reflection (albedo), how much more sunlight might you expect to receive at the surface of Venus? How much less light might you expect to receive at the surface of Mars? (Hint: use equation 1 and remember the denominator is the ratio of the distances) Light intensity of x = Light Xo intensity of standard / (ratio of the distance of X divided by standard Xo)2 Light Venus= 1366/ (.72) 22 = 2635 Watts/M2 Light at Venus is 2635/1366 = 92% greater than Earth Light Mars = 1366/(1.52) 2 = 591 Watts/M2 Light at Mars is 591/1366 = 43% less than Earth Revised on 10/26/2010 Page 1 of 1 In our model, the light source is 200 cm from the globe, and the globe has a radius of 15 centimeters. A flea sitting on the globe is 15 cm closer to the light source at noon than he is at sunrise or sunset. How much does the light intensity drop as our flea is rotated from noon to sunset? (Hint: use equation 1 again). Light @ 185 = Light at 200/(185/200) 2 = Light at 200/(.925) 2 = Light at 200/.856 if the light at 200 = 1 then 1/.856 = 1.16 the light intensity drops by 16% The sun is 150 million kilometers from the Earth, and the Earth’s equatorial radius is 6378 km. How much would you expect the sun’s intensity to drop, based only on this additional distance? (Hey, how about using equation 1 again). Light @ 185 = Light at Earth Surface/(150,000,000/150,006,378) 2 = Light at X/(.99999) 2 = Light at X/.99999 if the light at Earth’s closest point = 1 then 1/.9999 = 1.000 drops by 0% The amount of light difference is very little (not significant). Revised on 10/26/2010 Page 2 of 2 B. Effect of latitude and season on incoming solar radiation Table two: Latitude of measurement Light intensity Axis vertical Axis tilted 90° N (north pole) 0 0 66.5° N (arctic circle) 13 1 45° N 24 12 23.5° N (T of Cancer) 29 24 0° (equator) 36 29 23.5° S (T of Capricorn) 30 36 How do the measurements compare between latitudes when the tilt of the globe is changed? What day(s) of the year are represented by the globe with its axis vertical? What day(s) are represented by the globe with its axis tilted?. With the Earth vertical, the Equator is closest to the light source and therefore is brightest. With the Earth tilted, the Tropic of Capricorn is closest to the light source and therefore is brightest. Axis tilted = Equinox (March 22 & Sept. 22) Axis vertical = 1st day of Summer/ winter (shortest & longest days of the year (June and Sept 22) Compare the decrease in light intensity from the equator to 23.5 N with the decrease between 45° N and 66.5° N. Since the changes in latitude are similar, why is the change in intensity so much different? The angle at which the sun’s rays strike the globe is different. Revised on 10/26/2010 Page 3 of 3 In the northern hemisphere winter, Earth is near perihelion (closest approach to the sun), at 147 million km, while during the northern hemisphere summer Earth is at aphelion (furthest from the sun) at 152 million km. Why are the summers hotter than the winters in the northern hemisphere? The tilt of Earth’s axis is more significant than the elliptical orbit. C. Albedo Incident Light 320 Table three: Surface White Black Water Ice Reflected Radiation 60 7 10 40 Albedo (equation 2) 18% 2% 3% 12.5% If you had a lava flow made of fresh, black basalt partially covering a light-colored granite surface, which rock would have the greater albedo? What happens to the radiation that is incident to the surface but is not reflected back into the atmosphere (hint: think about walking across an asphalt parking lot in bare feet in the summer.)? The light colored rock has the greater albedo (reflectivity). Heat is absorbed by the darker color. Revised on 10/26/2010 Page 4 of 4 Which surface was more reflective, the water or the ice? If continental glaciers and sea ice were to begin to expand on the Earth at the expense of rock and ocean, what effect might this have on global temperatures? Currently, as glaciers melt and sea ice retreats further into the arctic regions each year, what effect are we likely to see on global temperatures? Ice has a much higher albedo. If ice expands, so does albedo hence more light is reflected and global temperatures would drop. As ice retreats, global temperatures will rise. On the diagram below, sketch the earth's axis at the winter and summer solstice, and indicate at what latitude the solar constant is at maximum during these periods. Would the earth's albedo be higher or lower in the southern hemisphere compared with the northern hemisphere? Explain! (hint: consider the distribution of land mass/water in the two hemispheres) The albedo in the southern hemisphere would be lower because a higher percentage of the Earth’s surface is ocean than in the north. Water absorbs rather than reflects light. Revised on 10/26/2010 Page 5 of 5 C. Turbidity in Seawater Table four: Sediment concentration Light intensity (lux) Visibility limit (cm) 0 grams 326 60 cm 1 gram (50 mg/liter) 23 54 2 gram (100 mg/liter) 7 27 3 gram (150 mg/liter) 4 16 Which is the more accurate measure of turbidity: measuring light loss with the lux meter, or using the mini Secchi disk? Explain! Measuring with the Lux Meter is theoretically more accurate because it measures light in the same way every time (unless the batteries are weak or there is contamination on the sensitive meter. Also, you may see the Secchi disk differently than your partner because the eyesight of individuals differs. However, many of you did very well with the Secchi disk! Revised on 10/26/2010 Page 6 of 6 Suppose rather than fine grained clay/silt sized particles, you had added the same concentrations (50 mg/liter, 100 mg/liter, and 150 mg/liter) of sand sized particles to the aquarium. Would you expect the turbidity (i.e., light attenuation) to be the same, greater, or less? Explain! At first, the light attenuation may be the same (fewer large particles versus more small particles,) but settling would occur much more quickly with the sand and so the water would clear faster. C. Light Attenuation and settling rates Table five: Time Light intensity (lux) Suspended sediment (mg) 0 minutes 2 150 1 minutes 4 145 2 minutes 6 137 3 minutes 9 117 4 minutes 10 114 5 minutes 11 112 6 minutes 12 110 7 minutes 13 104 8 minutes 13 104 9 minutes 14 100 10 minutes 14 100 Revised on 10/26/2010 Page 7 of 7 From your laboratory experiments, can you tell if water with higher suspended sediment concentrations would heat up faster than clear water? Explain! (Hint: consider the light absorption experiments, not the albedo!) As the sediments absorb light the water should heat up faster. Light is energy; light is absorbed and converted to heat. However, the temperature may not rise much because of water’s high heat capacity. Examine the Sediment Concentration vs. Time Graph below. This settling graph is similar to your laboratory experiment. Which of the two curves (A or B) represents the coarser sediment? Explain! B settles faster and is therefore coarser. Revised on 10/26/2010 Page 8 of 8 Primary productivity is enhanced by light. The depth of the photic zone is measured by the depth of light penetration. Can productivity affect the depth of the photic zone? Explain! Yes, productivity affects the depth of the photic zone. High productivity means “more plankton”; more plankton absorb and reflect more light. So the light does not penetrate as deeply when productivity is high. Revised on 10/26/2010 Page 9 of 9
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