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Vaisakh Gopinathan
FRM-PA3-01
“Emulating natural upwelling”
13/01/14
 Acts like a ‘biological pump’ encourages the
growth of lush oceanic pastures
 The divergence of currents that bring deeper,
colder, nutrient rich waters to the surface
W E
 Bringing relatively nutrient-rich deep water
(>200m) to the surface ocean
 Stimulate phytoplankton activity
 Draw down atmospheric carbon dioxide
 Productive coastal upwelling area - 1% of total
ocean area
 90% of the ocean area is considered as biological
deserts
 Artificial upwelling helps to enhance primary
production in these areas
 Ocean thermal energy conversion
(OTEC):
• Temperature difference of 20 degree C
between upper and bottom layers
• Upwelling as byproduct, mainly to
produce electricity
 The cold and nutrient rich water is pumped from the
deeper ocean layer to the condensor
 The water is poured back to the surface layer after
use
 Hence the nutrients will reach the surface layer
• Used in ocean deserts
• Upwelling occurs due to
temperature and salinity
gradients between the upper
and bottom layers of water
• Vertical motion by buoyant
force
 Model used in the open ocean off the
south coast of Oahu
 Single device with a buoy 4.0 meters in
diameter and a tail pipe 300 meters long
and 1.3 meters in diameter
 It could generate a flow of about 1.0
cubic meter per second in random
waves.
 This rate is sufficient to develop DOW-
enhanced open ocean mariculture.
 The control will open upward only,
preventing the cold water from
backward flow
 Deployment of thousands of
plastic tubes (~300-600 feet long
and ~30 feet in diameter)
 Bridging the nutrient poor
surface water and the colder
nutrient rich surface water
 By pumping water to the deeper layer of fjords,
mainly in summer
 The submerged water bring the nutrients trapped
in bottom layer to the surface
 To enhance primary production, reduce the growth
of toxic algae etc.
 A wave driven pump to lift the deep, cool water to
the surface and enhance ocean fertility
 It sinks the hot surface water like a siphon and
exploit the gravity to drain the hot water to bottom
layers
 The warm water reaches the depth will mix with
cold water and rise outside the tube
 Brings the nutrient rich water to surface
 Enhance the open ocean mariculture
 Cost is high
 Corrosion problem
 Stress at the ocean conditions
The potential benefit from the concept is
enormous
To be formulate at low cost and high flow rate
OTEC good for larger installations, while
wave powered inertia pump is much simpler
 Muni Krishna, K., 2008. Coastal upwelling along the
southwest coast of India – ENSO modulation Ann.
Geophys., 26: 1331–1334
 http://www.energinat.com/future_upwelling.shtml
 Karl, D. M., Letelier, R. M., 2008. Nitrogen fixation-
enhanced carbon sequestration in low nitrate, low
chlorophyll seascapes. Mar Ecol Prog Ser 364: 257-268
 White, A., Karin B., David K. and Eric G., 2009. An Open
Ocean Trial of Controlled Upwelling Using Wave Pump
Technology. J. Atmo. and Oce. Tech., 10. pp 1175
 Shigenao, M., Koutaro, T., Keisuke T. and Seigo, S. , 2004
Artificial Upwelling of Deep Seawater Using the Perpetual
Salt Fountain for Cultivation of Ocean Desert. Journal of
Oceanography, Vol. 60, pp. 563 to 568
 http://curry.eas.gatech.edu/Courses/6140/ency/Chapter2/
 www.esru.strath.ac.uk/EandE/Web_sites/02-03/ocean_the
 Stommel, H., Arons, A. B. and Blanchard, D. ,1956.
An ocean curiosity: the perpetual salt fountain.
Deep-Sea Res., 3. 152-153
 Liu, C. C. K. and Qiao, J., 1995. Artificial upwelling in
regular and random waves. Ocean Engng., 22(4).
337-350
Open for discussion…
For your kind attention…

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Artificial Upwelling

  • 2.  Acts like a ‘biological pump’ encourages the growth of lush oceanic pastures
  • 3.
  • 4.
  • 5.
  • 6.  The divergence of currents that bring deeper, colder, nutrient rich waters to the surface
  • 7. W E
  • 8.
  • 9.
  • 10.
  • 11.  Bringing relatively nutrient-rich deep water (>200m) to the surface ocean  Stimulate phytoplankton activity  Draw down atmospheric carbon dioxide
  • 12.  Productive coastal upwelling area - 1% of total ocean area  90% of the ocean area is considered as biological deserts  Artificial upwelling helps to enhance primary production in these areas
  • 13.  Ocean thermal energy conversion (OTEC): • Temperature difference of 20 degree C between upper and bottom layers • Upwelling as byproduct, mainly to produce electricity
  • 14.  The cold and nutrient rich water is pumped from the deeper ocean layer to the condensor  The water is poured back to the surface layer after use  Hence the nutrients will reach the surface layer
  • 15. • Used in ocean deserts • Upwelling occurs due to temperature and salinity gradients between the upper and bottom layers of water • Vertical motion by buoyant force
  • 16.  Model used in the open ocean off the south coast of Oahu  Single device with a buoy 4.0 meters in diameter and a tail pipe 300 meters long and 1.3 meters in diameter  It could generate a flow of about 1.0 cubic meter per second in random waves.  This rate is sufficient to develop DOW- enhanced open ocean mariculture.  The control will open upward only, preventing the cold water from backward flow
  • 17.
  • 18.  Deployment of thousands of plastic tubes (~300-600 feet long and ~30 feet in diameter)  Bridging the nutrient poor surface water and the colder nutrient rich surface water
  • 19.  By pumping water to the deeper layer of fjords, mainly in summer  The submerged water bring the nutrients trapped in bottom layer to the surface  To enhance primary production, reduce the growth of toxic algae etc.
  • 20.
  • 21.  A wave driven pump to lift the deep, cool water to the surface and enhance ocean fertility  It sinks the hot surface water like a siphon and exploit the gravity to drain the hot water to bottom layers  The warm water reaches the depth will mix with cold water and rise outside the tube  Brings the nutrient rich water to surface
  • 22.
  • 23.
  • 24.
  • 25.
  • 26.  Enhance the open ocean mariculture
  • 27.
  • 28.
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  • 31.  Cost is high  Corrosion problem  Stress at the ocean conditions
  • 32. The potential benefit from the concept is enormous To be formulate at low cost and high flow rate OTEC good for larger installations, while wave powered inertia pump is much simpler
  • 33.  Muni Krishna, K., 2008. Coastal upwelling along the southwest coast of India – ENSO modulation Ann. Geophys., 26: 1331–1334  http://www.energinat.com/future_upwelling.shtml  Karl, D. M., Letelier, R. M., 2008. Nitrogen fixation- enhanced carbon sequestration in low nitrate, low chlorophyll seascapes. Mar Ecol Prog Ser 364: 257-268  White, A., Karin B., David K. and Eric G., 2009. An Open Ocean Trial of Controlled Upwelling Using Wave Pump Technology. J. Atmo. and Oce. Tech., 10. pp 1175  Shigenao, M., Koutaro, T., Keisuke T. and Seigo, S. , 2004 Artificial Upwelling of Deep Seawater Using the Perpetual Salt Fountain for Cultivation of Ocean Desert. Journal of Oceanography, Vol. 60, pp. 563 to 568
  • 34.  http://curry.eas.gatech.edu/Courses/6140/ency/Chapter2/  www.esru.strath.ac.uk/EandE/Web_sites/02-03/ocean_the  Stommel, H., Arons, A. B. and Blanchard, D. ,1956. An ocean curiosity: the perpetual salt fountain. Deep-Sea Res., 3. 152-153  Liu, C. C. K. and Qiao, J., 1995. Artificial upwelling in regular and random waves. Ocean Engng., 22(4). 337-350
  • 35. Open for discussion… For your kind attention…