2Presentation Points Mechanisms that create ocean upwelling Types of upwellingIdentifying upwelling on satellite-derived mapsEcological and economic effects of upwelling
3Mechanisms that create ocean upwelling WindCoriolis EffectEkman Transport
4Upwelling refers to deep water that is brought to the surface. Areas of upwelling are created by surface winds that pull water away from an area. This deficit of water on the surface invites water to come up from deeper regions.
5To understand upwelling, you must be familiar with how the Coriolis Force affects ocean surface currents. The Coriolis Effect acts on moving water, because it is not attached to the rotating Earth. As water flows over the rotating earth, it appears to deflect to the right in the Northern Hemisphere and the left in the Southern.
6Due to friction between the layers of water in the ocean and the Coriolis Effect, the net result of wind blowing across the surface of the water is transportation of a layer of water 90 degrees to the direction of the wind. This is known as Ekman Transport.
11What’s the difference between Peru(A) and Columbia (B)?
123. Seasonal upwellingWindWindOnshore winds pile water up on shore, thus surface water will be forced downward. This is ‘downwelling’.Offshore winds take water away from shore, thus water from depth will upwell to the surface.
13The Monsoonal wind shifts in Oman create very different conditions. April, 1999Onshore winds: DownwellingAugust, 1999Offshore winds: Upwelling
14Identifying upwelling on satellite-derived maps Sea Surface TemperatureOcean Color
15The deep water that surfaces in upwelling is cold; by looking at Sea Surface Temperature maps we can identify cool upwelled water versus hotter surface water.
16Upwelled water also contains nutrients (nitrate, phosphate, silicate) and dissolved gases (oxygen and carbon dioxide) that are not utilized at depth because of a lack of sunlight. Now on the surface, these nutrients and gases help to fuel photosynthesis by small algae called phytoplankton.
17Phytoplankton photosynthesize using specialized color pigments called chlorophyll. Thus, “Ocean Color” maps are another way to identify areas of upwelling. Where on this ocean color map are high phytoplankton concentrations?
18Ecological and Economic effects of upwelling: Upwelling leads to more phytoplanktonMore phytoplankton leads to more fishMore fish lead to commercial fishing jobs and to more seafood
19Phytoplankton come in many shapes and forms Phytoplankton come in many shapes and forms. Collectively they form the base of oceanic food webs.Without upwelling many of the world’s fisheries would not thrive.
20Some climatic events can reduce upwellings. ~El Nino
21Along Peru’s coast, an El Nino event decreases the coastal winds Along Peru’s coast, an El Nino event decreases the coastal winds. Thus the upwelling from below is slowed.An El Nino condition results from weakened trade winds in the western Pacific Ocean near Indonesia, allowing piled-up warm water to flow toward South America.
22Even though upwelling areas account for only 1% of the ocean surface, they support 50% of the worlds fisheries.
23Productivity (phytoplankton growth) of an area is determined by the rate and the duration of upwelling.Rate of upwelling determines phytoplankton cell size.Duration of upwelling determines the total amount of phytoplankton.small vs. largefew vs. many
24Classification of upwelling systems in terms of rate and duration: Low Medium HighRATEDURATIONLong ShortAfter Thurman, H.V. (1994)
25Moderate rates of upwelling for long duration (8 months or longer) provide the ultimate combination for a large fishery.With too low or too high a rate, phytoplankton are small, so there is a trophic level between the algae and the fish….therefore the fish receive less energy.
26Upwelling and Fisheries JanuaryAprilJulyOctoberUsing this series of Sea Surface Temperature Maps from 1999, can you determine areas/times for possible fisheries?(Hint: Look at Peru’s coast in January and April. Look at the northwestern tip of Africa in July and October.)