With perhaps 6000 tonnes of helium per year getting produced, and the
moon continually tidal modulating Earth; its hot innards of gasses and
solids has to go somewhere.

On Mar 22, 2:42 am, Andrew Lockley <[email protected]> wrote:
> http://planetearth.nerc.ac.uk/news/story.aspx?id=1416&cookieConsent=A
>
> NEWS
>
> Icelandic volcano's ash led to more CO2 being absorbed by oceans
>
> 22 March 2013, by Harriet Jarlett
>
> The Icelandic volcano's ash plume that caused huge air travel disruption
> across Europe in 2010 resulted in the oceans absorbing more carbon dioxide
> (CO2) than usual, say scientists.
>
> They found that particles from the ash cloud that fell into the ocean
> provided microscope plants, called phytoplankton, with a nutrient boost in
> the form of iron. Phytoplankton are important as they absorb CO2 from the
> atmosphere. In fact, while phytoplankton represent just two per cent of all
> plant matter on Earth, they account for half of all CO2absorption from the
> atmosphere.'This had never been done, no one has ever made any at-sea
> in-situ measurements during an eruption,' explains Professor Eric
> Achterberg, from the National Oceanography Centre Southampton, lead
> researcher on the study.In the oceans south of Iceland there isn't usually
> enough iron for phytoplankton to bloom for more than a few weeks before it
> runs out. This latest study reveals that the volcanic ash column supplied
> enough iron that the phytoplankton were able to bloom for longer, and
> absorb more CO2 than they would typically have been able to.'In normal
> years the iron levels are very low in the Iceland basin as the system runs
> out of this nutrient during the annual spring bloom. But in 2010 the iron
> supply was so high that demands were met. But then the phytoplankton
> stripped the nitrogen out of the surface waters so they became limited by
> that instead,' says Achterberg.The research, published in Geophysical
> Research Letters, found even with the added iron from the volcano and the
> longer blooming period, the phytoplankton were only able to absorb about
> 15-20 per cent more CO2 than in other years before the nitrogen in the
> water ran out.Intentionally adding iron to the oceans, called iron
> fertilisation, has been suggested as a way of getting phytoplankton to
> bloom and absorb more carbon dioxide, to combat rising levels in the
> atmosphere.The results in the study were collected on three separate
> expeditions on the RRS Discovery. Eyjafjallajökull erupted just as the
> first cruise was about to embark and nearly spelled the end of several
> long-planned experiments - scientists had originally intended to observe
> the normal iron levels in the water and see if phytoplankton struggle to
> find enough iron.But then the researchers became the first to measure the
> effect of a volcanic eruption on the ocean productivity, whilst the
> eruption was happening. 'We managed to get right under the plume. We
> sampled there to look at the effects of ash on the water column and see how
> it affected dissolved iron and aluminium concentration. It was challenging
> - the ship was covered with ash,' concludes Achterberg.
>
> Achterberg, E. P., C. Mark Moore, S. A. Henson, S. Steigenberger, A. Stohl,
> S. Eckhardt, L. C. Avendano, M. Cassidy, D. Hembury, J. K. Klar, M. I.
> Lucas, A. I. Macey, C. M. Marsay, and T. J. Ryan-Keogh (2013), Natural iron
> fertilization by the Eyjafjallajökull volcanic eruption, Geophys. Res.
> Lett., 40, doi:10.1002/grl.50221.
>
> Keywords: Biology, Climate system, Earth system, Environmental
> change,Hazards, Marine life, Plants, Volcanoes, Water,

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