Since phytoplankton form the base of marine food webs, the world's most productive fisheries are located in areas
of coastal upwelling that bring cold nutrient rich waters to the surface (especially in the eastern boundary regions of the subtropical gyres); about half the world's total fish catch comes from upwelling zones.
The two big surprises to surface recently are acidification and perturbation
of coastal upwelling ecosystems.
This freshwater creates a lens on the Gulf surface as well as the cooling effects
of coastal upwelling due to wind stress.
«Areas of greatest vulnerability will likely be where deep waters, naturally low in pH, meet acidified surface waters,» such as areas
of coastal upwelling along the West Coast and in estuary environments such Hood Canal, the new study predicts.
The waters probed during this study, known as the California Current, are a hot spot of ocean acidification because
of coastal upwelling, which brings naturally acidic waters to the surface, where they are made even more acidic by greenhouse gas pollution.
Not exact matches
This is not only because harvesting from relatively shallow waters is easier than in the open ocean, but also because fish are much more abundant near the
coastal shelf, due to
coastal upwelling and the abundance
of nutrients available there.
The winds drove westward Ekman transport, which induced a geostrophic northward
coastal current (20 cm / s) off the western coast
of Wilhelmina Bay and
upwelling at its southern and eastern margins.
Global climate change and intensification
of coastal ocean
upwelling.
Greenhouse gas,
upwelling - favorable winds, and the future
of coastal ocean
upwelling ecosystems.
My understanding
of this process is that it mostly occurs near
coastal upwellings which bring up nutrients from the deep and that it is responsible for a significant fraction
of ocean carbon sequestration.
There was little
coastal upwelling on the Pacific coast (
of North America at least) and I believe several other oceanographic features mimicked El Nino.
The
coastal wind driven
upwellings are well known and they drive a good proportion
of the world's shipping industry.
The wind driven
coastal upwellings are a tiny fraction
of the ocean surface and volume.
Collectively,
coastal upwelling ecosystems represent only 1 %
of the surface waters
of the ocean, but they have historically provided 20 %
of the fisheries.
Furthermore, during the peak
of the
upwelling season (May - June), central and northern California Current
coastal waters returned to normal temperatures as cold water was brought to the surface.
Inshore
of this a
coastal component exhibits dynamic wind - driven
upwelling, which is strongly modulated by local weather systems, resulting in short - term
upwelling cycles with a periodicity
of 5 — 10 days.
The most productive
coastal upwelling area
of the modern ocean is the Benguela
upwelling system off south - western Africa, an area that is considered to represent an important modern analogue
of petroleum source rocks deposited in the geological past.
report that ocean sediment cores containing an «undisturbed history
of the past» have been analyzed for variations in PP over timescales that include the Little Ice Age... they determined that during the LIA the ocean off Peru had «low PP, diatoms and fish,» but that «at the end
of the LIA, this condition changed abruptly to the low subsurface oxygen, eutrophic
upwelling ecosystem that today produces more fish than any region
of the world's oceans... write that «in
coastal environments, PP, diatoms and fish and their associated predators are predicted to decrease and the microbial food web to increase under global warming scenarios,» citing Ito et al..
Upwelling creates areas
of cold
coastal surface waters that stabilize the lower troposphere and reduce the chances for convection.
Thus the topography
of the
coastal shelves and depth
of submerged glacier grounding points determines the impact
of upwelled CDW and limits extreme basal melting to a relatively few locations as illustrated by the red and orange areas in the figure below (from Depoorter 2013)..
In Washington and Oregon, oysters farms are in
coastal Pacific waters where
upwelling currents are bringing up cold, deep water with higher amounts
of CO2 and a more acidic pH. Watch and listen to two oyster farmers from Taylor Shellfish Farms in Washington state talk how about ocean acidification is impacting their young oysters.
«Changes in basal melting are helping to change the properties
of Antarctic bottom water, which is one component
of the ocean's overturning circulation,» said author Stan Jacobs, an oceanographer at Columbia University's Lamont - Doherty Earth Observatory in Palisades, N.Y. «In some areas it also impacts ecosystems by driving
coastal upwelling, which brings up micronutrients like iron that fuel persistent plankton blooms in the summer.»
Additionally, decreasing shell δ13C at Tatoosh Island is consistent with
upwelling of younger water, as if fossil fuel CO2 were invading the
coastal waters both from the atmosphere and, increasingly, through the thermocline.
Accordingly,
upwelling of waters acidified by anthropogenic CO2 has led to a further decrease in surface pH, as reported in the eastern Pacific Ocean along the west coast
of North America, from central Canada to northern Mexico, where shoaling
of the layer
of seawater undersaturated with aragonite increased the frequency and magnitude
of coastal acidification associated with
upwelling events (Feely et al. 2008, 2010).
However, the conditions predicted for the open ocean may not reflect the future conditions in the
coastal zone, where many
of these organisms live (Hendriks et al. 2010a, b; Hofmann et al. 2011; Kelly and Hofmann 2012), and results derived from changes in pH in
coastal ecosystems often include processes other than OA, such as emissions from volcanic vents, eutrophication,
upwelling and long - term changes in the geological cycle
of CO2, which commonly involve simultaneous changes in other key factors affecting the performance
of calcifiers, thereby confounding the response expected from OA by anthropogenic CO2 alone.
The
coastal upwelling is a rather stable feature
of large scale ocean dynamics.
That
coastal upwelling of ocean water would increase.
The California Current System (CCS) contains one
of the five major
coastal upwelling zones in the world's oceans, and hosts a great diversity and abundance
of marine life [1].