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Storms fuel blooms of marine plants

Date:
November 3, 2015
Source:
National Oceanography Centre
Summary:
Autumn storms help the ocean absorb atmospheric carbon dioxide and stimulate marine life by ‘stirring-up’ the nutrients that feed blooms of tiny marine plants. These microscopic marine plants, or phytoplankton, play a key role in moving carbon dioxide from the atmosphere into the deep ocean, as well as forming the base of the marine food-web. To fuel their growth they absorb atmospheric carbon dioxide and nutrients from the top hundred meters of the ocean. This depletes the upper ocean of nutrients. Understanding the processes of replenishment has preoccupied oceanographers for generations, partly because of suggestions that global environmental change might suppress it.
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Autumn storms help the ocean absorb atmospheric CO₂ and stimulate marine life by 'stirring-up' the nutrients that feed blooms of tiny marine plants.

Anna Rumyantseva, the lead author of this research at the National Oceanography Centre (NOC), said "By learning more about what encourages the growth of these greenhouse gas absorbing blooms, this finding contributes to a growing understanding of the importance of the ocean in global environmental change."

These microscopic marine plants, or phytoplankton, play a key role in moving CO₂ from the atmosphere into the deep ocean, as well as forming the base of the marine food-web. To fuel their growth they absorb atmospheric CO₂ and nutrients from the top hundred metres of the ocean. This depletes the upper ocean of nutrients. Understanding the processes of replenishment has preoccupied oceanographers for generations, partly because of suggestions that global environmental change might suppress it.

Writing in Global Biogeochemical Cycles, Anna describes how storms drive turbulence in the ocean causing nutrients to 'well-up' from the deep. This process can result in up to a tenfold increase in nutrient concentrations in the surface layers of the ocean during a storm. Subsequent measurements of small turbulent structures within the ocean enabled scientists to quantify the 'stirring-up' of nutrients resulting from the interaction between storm winds and currents. A few days afterwards scientists measured a fifty percent rise in the concentration of chlorophyll, which suggests phytoplankton numbers had increased.

Although storms can promote phytoplankton blooms in autumn, in spring the situation is reversed. Because phytoplankton blooms in spring are stimulated by light, rather than nutrients, storm induced mixing can suppress blooms by pulling phytoplankton deeper into the ocean where there is less light.

This study is the first that has linked storms and 'marine productivity' in the northern North Atlantic due to the challenges of conducting ship-based measurements during storms. The team at the NOC solved this problem by using robotic gliders, which can continue to take measurements regardless of the weather.

Dr Stephanie Henson (NOC), who co-authored this paper said "Technology such as robotic gliders is enabling scientists to take measurements in places, and at times, that have previously been out-of-reach."


Story Source:

Materials provided by National Oceanography Centre. Note: Content may be edited for style and length.


Journal Reference:

  1. Anna Rumyantseva, Natasha Lucas, Tom Rippeth, Adrian Martin, Stuart C. Painter, Timothy J. Boyd, Stephanie Henson. Ocean nutrient pathways associated with the passage of a storm. Global Biogeochemical Cycles, 2015; 29 (8): 1179 DOI: 10.1002/2015GB005097

Cite This Page:

National Oceanography Centre. "Storms fuel blooms of marine plants." ScienceDaily. ScienceDaily, 3 November 2015. <www.sciencedaily.com/releases/2015/11/151103090539.htm>.
National Oceanography Centre. (2015, November 3). Storms fuel blooms of marine plants. ScienceDaily. Retrieved May 23, 2017 from www.sciencedaily.com/releases/2015/11/151103090539.htm
National Oceanography Centre. "Storms fuel blooms of marine plants." ScienceDaily. www.sciencedaily.com/releases/2015/11/151103090539.htm (accessed May 23, 2017).

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