1 00:00:00,000 --> 00:00:04,000 Hi, I'm Dr. Martins. Glad you found me. 2 00:00:04,000 --> 00:00:10,000 Hi, Dr. Martins. Dr. D told us that the density of water depends upon its temperature and salinity. 3 00:00:10,000 --> 00:00:13,000 But how does temperature make the water more dense? 4 00:00:13,000 --> 00:00:18,000 Cold water molecules are packed together more tightly than warm ones, making cold water denser. 5 00:00:18,000 --> 00:00:22,000 So do the density currents form near the north and south poles? 6 00:00:22,000 --> 00:00:27,000 Exactly. The cold air at the poles cools the surface water, making it denser and causing it to sink. 7 00:00:27,000 --> 00:00:29,000 What about salinity? 8 00:00:29,000 --> 00:00:35,000 When ice forms in polar waters, it leaves behind salt, which increases the salinity of surrounding water. 9 00:00:35,000 --> 00:00:38,000 The higher salt content makes the polar water denser. 10 00:00:38,000 --> 00:00:41,000 I learned that evaporation also makes water saltier. 11 00:00:41,000 --> 00:00:46,000 That's right. In areas such as the Mediterranean Sea, where there's little rainfall and lots of heat, 12 00:00:46,000 --> 00:00:50,000 evaporation removes fresh water and leaves extremely salty water. 13 00:00:50,000 --> 00:00:52,000 Where does the denser water go? 14 00:00:52,000 --> 00:00:55,000 The denser polar water sinks and creates the thermohaline circulation. 15 00:00:55,000 --> 00:00:57,000 Thermohaline? 16 00:00:57,000 --> 00:01:00,000 Thermal for temperature and haline for salinity. 17 00:01:00,000 --> 00:01:05,000 The cold, salty water masses that create this circulation form in only two places. 18 00:01:05,000 --> 00:01:11,000 The water mass sinking off Greenland is called the North Atlantic Deep Water, or NADW. 19 00:01:11,000 --> 00:01:16,000 The water mass sinking off Antarctica is called the Antarctic Bottom Water, or AABW. 20 00:01:16,000 --> 00:01:18,000 Where do these currents end up? 21 00:01:18,000 --> 00:01:24,000 They both sink down several kilometers while spreading out horizontally and moving along the bottom of the Atlantic Ocean. 22 00:01:24,000 --> 00:01:27,000 They eventually mix while circulating around Antarctica. 23 00:01:27,000 --> 00:01:31,000 Then they move into the deep Indian Ocean and finally into the Pacific. 24 00:01:31,000 --> 00:01:35,000 So the water from the poles may one day end up on a beach in Hawaii? 25 00:01:35,000 --> 00:01:37,000 I guess you can look at it like that. 26 00:01:37,000 --> 00:01:39,000 What goes down must come up. 27 00:01:39,000 --> 00:01:43,000 It takes the average water molecule a thousand years to make the complete cycle. 28 00:01:43,000 --> 00:01:45,000 Wow, that's a long time. 29 00:01:45,000 --> 00:01:50,000 Yes, we call the cycle the Global Conveyor Belt, and it has a large impact on climate. 30 00:01:50,000 --> 00:01:53,000 I went swimming once, and the water was really cold. 31 00:01:53,000 --> 00:01:56,000 My mom said it was an upwelling, but what's that? 32 00:01:56,000 --> 00:02:00,000 The coastal upwelling that you experienced is different from thermohaline circulation. 33 00:02:00,000 --> 00:02:03,000 It only brings up cold water from a few hundred meters deep. 34 00:02:03,000 --> 00:02:07,000 It's also not as cold as AABW or NADW. 35 00:02:07,000 --> 00:02:10,000 Coastal upwelling is generally caused by wind. 36 00:02:10,000 --> 00:02:11,000 Is upwelling important? 37 00:02:11,000 --> 00:02:12,000 Good question. 38 00:02:12,000 --> 00:02:15,000 Upwelling brings lots of nutrients up from deep water. 39 00:02:15,000 --> 00:02:20,000 We are researching the impact of nitrogen, a crucial nutrient, on Florida Keys reefs. 40 00:02:20,000 --> 00:02:22,000 How does upwelling affect the reef? 41 00:02:22,000 --> 00:02:28,000 It appears that there have been major changes in the health and community structure of coral reefs here in the Keys and throughout the world. 42 00:02:28,000 --> 00:02:34,000 By observing the nitrogen composition of sponges, we can determine the importance of different nitrogen sources. 43 00:02:34,000 --> 00:02:36,000 Wow, you've given us a lot to think about. 44 00:02:36,000 --> 00:02:37,000 Thanks, Dr. Martens. 45 00:02:37,000 --> 00:02:39,000 You're welcome. Good luck on your project.