Collectively, coastal
upwelling ecosystems represent only 1 % of the surface waters of the ocean, but they have historically provided 20 % of the fisheries.
The two big surprises to surface recently are acidification and perturbation of coastal
upwelling ecosystems.
The Humboldt Current Large Marine Ecosystem (off Chile and Peru), the Benguelan Current LME (Namibia and South Africa), the Canary Current LME (Morocco), are the other main
upwelling ecosystems, all driven by similar oceanographic and atmospheric processes, all on the eastern sides of ocean basins (western sides of continents).
Greenhouse gas, upwelling - favorable winds, and the future of coastal ocean
upwelling ecosystems.
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..
Not exact matches
This
ecosystem, which alone provides 5 to 10 % of the world's catches, owes its exceptional productivity to the nutrients provided by
upwellings of deep, cold, nutrient - rich water along the coasts.
As Dr. Mackey cited in the published article Sea Change: UCI oceanographer studies effects of global climate fluctuations on aquatic
ecosystems: «They would tell us about
upwelling and how the ocean wasn't just this one big, homogenous bathtub, that there were different water masses, and they had different chemical properties that influenced what grew there,» she recalls.
That kept deep, nutrient - rich water from reaching the surface — an
upwelling that serves as «a kind of turbo boost to the
ecosystem,» Parrish says.
Coastal
ecosystems can experience acidification via
upwelling, eutrophication, riverine discharge, and climate change.
The prevailing California Current flows southward along the coast, causing an
upwelling of nutrient - rich water that provided the foundation for the area's marine
ecosystem.
In normal years, spring and summer winds lead to
upwelling of cold, nutrient - rich waters at the coast, fueling the highly productive California Current
ecosystem.
In South Africa, fisheries could be affected by changes in estuaries, coral reefs and
upwelling; with those that are dependent on the first two
ecosystems being the most vulnerable (Clark, 2006).
I hypothesized here «that
upwelling in the Pacific Ocean is modulated by solar activity over periods of decades to millennia — with profound impacts on communities and
ecosystems globally.
«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.»
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.
Upwelling - driven nearshore hypoxia signals
ecosystem and oceanographic changes in the northeast Pacific
Substantial biodiversity exists in both pelagic and benthic realms and along coastlines, in a diverse range of
ecosystems from highly productive (e.g.,
upwelling regions) to those with low productivity (e.g., oceanic gyres).