Question: On Which Of The Following Currents Might You Predict That Upwelling Is An Important Process? Select ALL Correct Answers. You May Want To Consult The Map Below (on P. 177 Of Your Text) For Help, Though Not All The Currents Are Labeled. Att 29 5 5 MONTH Pen ATLANTIC Ww HOT MORE CHE INDIAN CREANOVE ATLANTEN M Major Warna Car Dience Re FIGURES We Went Of …

On which of the following currents might you predict that upwelling is an important process? Select ALL correct answers. You may want to consult the map below (on p. 177 of your text) for help, though not all the currents are labeled. Att 29 5 5 MONTH Pen ATLANTIC ww HOT MORE CHE INDIAN CREANOVE ATLANTEN M Major Warna Car dience re FIGURES We went of the dove dvergenees well. The me en fon whopilares both norm whether in who und here we are everyone within the eyes wwwser for de bewoners A Colo Cewe the storal the complicity in the North Temper. Der vil of the tween the while and conding Attention Antarctic Circumpolar Current Kuroshlo Current California Current Benguela Current Peru Current dor 19 NORTH PA ATLANTREN where C ENEN BCEANONE TRPAONGE NORTH ATLANTICO பல்aேl M Majer Maju warm curre coverace Cold currents divergence FIGURE 2 The wind-driven surface of these and the location of her convergence od divergences red. The surface was form wherealgyre hathat and south of the rise, and the tropical cover within the res Comences are also found at higher latitudes between the topical gyres and the Antarctic Circumpol Current, and between the tropical Aves with complicated histories in the Northermier Diverses on these of the stor between the shiropical wildung Antarctica Antarctic Circumpolar Current Kuroshio Current California Current Benguela Current Peru Current Gulf Stream Thermohaline circulation is driven by differences in water masses’ temperatures and salinities. resulting in differences in (answer1). SC Nor A She NaCl AW W War AM FIGURE 8-25 A vertical cross section of the Atlantic Ocean shows the various water masses that form layers at different depths. Antarctic Boston Water is the deniest water mass, and it Bows northward from around Antarctica North Atlantic Bottom Water sinks near Greenland and flows south ward over the top of Antarctic Bottom Water Intermediate-depth water masses are formed and sink at the Antarctic and subpolar convergence The near-surface luyen are more complex. Note the tongue of Mediterranean Water that spread across the North Atlantic Ocean from the Straits of Gibraltar at about 2000 10 3000 m depth between 20 and 55″N,