Global warming─Are humans responsible? Part 7 7.2 © Oxford University Press 2009 What is the normal global distribution pattern of temperature? Part A Quit Part 7 Global warming─Are humans responsible? What is the major factor affecting air Monthly mean temperatures temperature? What is the relationship between location and annual mean temperature of the Insolation. following three places? What makes the air temperature vary among latitudes and at different times of a year? © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 What is insolation? The sun is constantly releasing energy Solar in all directions. radiation In order to have a better This energy is understanding of the issue of as solar known global warming, we have to radiation. know more about insolation. Space The atmosphere Insolation Solar radiation that is received in the atmosphere or on the earth’s surface is known as insolation. Earth’s surface © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 What is insolation? Is insolation evenly distributed on the earth? Less insolation More insolation + Average annual insolation over the earth’s surface In general, insolation receivedon ( declines increases ) The distribution of insolation the earth’s/ surface with increasing latitude. is ( even / uneven ). © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 What is insolation? Is insolation evenly distributed on the earth? Why does insolation vary with latitudes? Average annual insolation over the earth’s surface The areas around _______ N and value S receive the highest Which areas receive the highest of insolation? value of insolation. © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 What is insolation? What factors affect insolation received on the earth’s surface? Factors affecting insolation received on the earth’s surface Angle of the sun Latitude © Oxford University Press 2009 Duration of daylight Time of a day The atmosphere Season Quit Global warming─Are humans responsible? Part 7 In Part B, we will discuss the relationship between insolation and air temperature. © Oxford University Press 2009 Quit Part 7 © Oxford University Press 2009 Global warming─Are humans responsible? Quit Global warming─Are humans responsible? Part 7 1 Angle of the sun The angle of the sun refers to the angle at which sunlight strikes the earth’s surface. When the sun is directly overhead, or when the angle of the sun is 90°, it is known as the overhead sun. Overhead sun Area A 90° angle / Right of angle Angle of the sun How does the the the Area to warm upsun affect Smaller intensity of insolation? Intensity of insolation © Oxford University Press 2009 High / More intense Area B < 90° / Acute angle Larger Low / Less intense Quit Global warming─Are humans responsible? Part 7 1 Angle of the sun A Latitude In low-latitude regions: The angle of sun is ( smaller / larger ). The insolation concentrates on a ( smaller / larger ) area. Therefore, the insolation is ( weaker / stronger ). (Credit: NASA) © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 1 Angle of the sun A Latitude In high-latitude regions: The angle of sun is ( smaller / larger ). The insolation concentrates on a ( smaller / larger ) area. Therefore, the insolation is ( weaker / stronger ). (Credit: NASA) © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 1 Angle of the sun B Time of a day The sun at noon is called the midday sun The amount The angle of sunof insolation received ( decreases / increases / in will be lower reacheswinter. maximum ) How is the amount of insolation received in this site different in winter? The angle of sun ( decreases / increases / reaches maximum ) The angle of sun ( decreases / increases / reaches maximum ) The amount of insolation received in a mid-latitude site in the Northern Hemisphere around the spring equinox © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 1 Angle of the sun C Season What is the relationship In spring summer autumnal winter solstice, equinox, solstice, equinox, the the between the the overhead overhead sunin sun is is seasons NS located atKong _______ the _________. Equator. Hong which _________. It Hong is the Kong isand time close Hong receives that to Equator insolation? Kong (Hong more Kong. receives Kong / less receives It is less ) the time( that the insolation leastHong in/ spring autumn largest Kong ) receives amount than in winter. summer. of the insolation. ( least / largest ) amount of insolation. Please click above for animation © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 2 Duration of daylight Is the case in The duration longer the ofduration daylight of in daylight, equatorial the regions ( less is/ almost more ) polar areas 12 insolation hours daily received. throughout a year. different? © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 2 Duration of daylight While in winter, In polar regions, there is no When does the North Pole receive daylight can last for 24 sunlight at all. the largest amount of insolation? hours in summer. © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 3 The atmosphere The dust particles, molecules andreaches clouds in Only about 58 unitsgas of solar radiation thethe earth’s atmosphere are able to reflect, absorb or scatter solar surface. radiation. How does the atmosphere affect the amount of solar radiation reaching the earth’s surface? © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 3 The atmosphere Why does the maximum insolation received occur at around N and S but not at the Equator? Maximum insolation received Maximum insolation received Maximum insolation received © Oxford University Press 2009 Quit Global warming─Are humans responsible? Part 7 3 The climate is drier and there is less cloud cover at around N and S. The earth’s surface receives more insolation, so the amount of insolation is greatest here. The atmosphere Space The atmosphere Less cloud cover Insolation is reflected by clouds Dense cloud cover The amount of cloud cover in the equatorial regions is high. Much of the solar radiation is reflected by clouds. This may reduce the amount of insolation reaching the earth’s surface. S © Oxford University Press 2009 0° Less cloud cover N Quit