18 Dey-Driven und 64 Deep-Water and Sha T 14 Cotal Pro 7 Open Compact of clos A Uping Doming, and Mae Ecotes and Food We

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18 Dey Driven Und 64 Deep Water And Sha T 14 Cotal Pro 7 Open Compact Of Clos A Uping Doming And Mae Ecotes And Food We 1 (33.48 KiB) Viewed 29 times

18 Dey-Driven und 64 Deep-Water and Sha T 14 Cotal Pro 7 Open Compact of clos A Uping Doming, and Mae Ecotes and Food Webe Primary Production The 154 108 TEA What does PS The Amern Conc 134 Change in t 128 The Oand Cimate Change 134 inviting the m 138 Sening the Upper O Type here to search Adobe Dighal Ed-Ocean Studies antigation 2021-2022 34 Om Sty and Denty AC Co 5. A secondary minor increase in production occurs in July August. What might be the cause of the change in production? Solar insolation is in August Nutrients recycled from the March production are recycled back into the water River influx is greatest during August after heavy rains 6. Bermuda is located in the Sargasso Sea within the North Atlantic subtropical gyre, where waters have relatively low total productivity The warm and saline surface waters typically are stratified all year so that spwelling and vertical moting are not factors in net primary production. The reason for the spring maxima in net production at 1 m and 40 m is likely due to that time of year & mixing due to tropical cycloors e increased nutrient intake from rivers 7. The subsequent decline until June in art primary production at near-surface waters (1m and 40m) is likely due to declining solar radiation & apply both a and bare conect & nutriezone 38 AD 1. A limiting factor in photosynthesis is the amount of sunlight available Solar radiation is attenuated by ocean water. Even in clear, clean ocean water, red light is completely absorbed within the first 15 m (49 ) of depth and typically only about 1% of absorbed sunlight reaches 150 m (492) depth. The section of water that light penetrates is called primary production 12:04 PM