Observational evidence for volcanic impact on sea level and the global water cycle

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Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008 Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008 Observational evidence Observational evidence for volcanic impact on for volcanic impact on sea level and the sea level and the global water cycle global water cycle 1. Arctic Centre, University of Lapland, Finland 1. Arctic Centre, University of Lapland, Finland 2. Thule Institute, University of Oulu, Finland 2. Thule Institute, University of Oulu, Finland 3. PSMSL, Proudman Oceanographic Laboratory, 3. PSMSL, Proudman Oceanographic Laboratory, Liverpool, UK Liverpool, UK Aslak Grinsted 1 , J. C. Moore 1,2 , S. Jevrejeva 3

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Observational evidence for volcanic impact on sea level and the global water cycle. Aslak Grinsted 1 , J. C. Moore 1,2 , S. Jevrejeva 3. 1. Arctic Centre, University of Lapland, Finland 2. Thule Institute, University of Oulu, Finland 3. PSMSL, Proudman Oceanographic Laboratory, Liverpool, UK. - PowerPoint PPT Presentation

Transcript of Observational evidence for volcanic impact on sea level and the global water cycle

Page 1: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Observational evidence for Observational evidence for volcanic impact on sea level volcanic impact on sea level and the global water cycleand the global water cycle

1. Arctic Centre, University of Lapland, Finland1. Arctic Centre, University of Lapland, Finland2. Thule Institute, University of Oulu, Finland2. Thule Institute, University of Oulu, Finland

3. PSMSL, Proudman Oceanographic Laboratory, Liverpool, UK3. PSMSL, Proudman Oceanographic Laboratory, Liverpool, UK

Aslak Grinsted1, J. C. Moore1,2, S. Jevrejeva3

Page 2: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

OutlineOutline

• Motivation• Objectives• Data• Approach• Results• Conclusion

Page 3: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Volcanoes and Climate

• Major volcanic eruptions can inject scattering aerosol into the stratosphere and thus impose a significant radiative cooling of the atmosphere.

MotivationMotivation

Page 4: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Volcanoes and ClimateVolcanoes and Climate

Source: Robock (2000) Volcanic eruptions and climate. Rev. Geophys.

Page 5: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Volcanoes and changes in ocean heat contentVolcanoes and changes in ocean heat content

Gleckler et al. Nature 2005

Lasting effect

From Hansen et al., 2002, JGR

Short term effect

Page 6: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Models of volcanic impact on sea levelModels of volcanic impact on sea level

Major volcanic eruption▼

Cooling of the world oceans▼

Densification▼

Sea level drop

Nature, 2005

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Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Observational verification?Observational verification?

Nature 2005

??

Can we quantify the impact of volcanic eruptions using observations?

Page 8: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Major contributors to sea level riseMajor contributors to sea level rise

Page 9: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

ObjectiveObjective

• Estimate the effect of volcanic eruptions on observational sea level.

Page 10: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Jevrejeva et al., Jevrejeva et al., Nonlinear trends and multi-year cycle in sea level records. Nonlinear trends and multi-year cycle in sea level records. Journal of Journal of Geophysical ResearchGeophysical Research, 111, 2005JC003229, 2006, 111, 2005JC003229, 2006. . Data: Data: www.pol.ac.uk/psmsl/author_archive/jevrejeva_et_al._jgr.htmlwww.pol.ac.uk/psmsl/author_archive/jevrejeva_et_al._jgr.html

Location of 1023 tide gauges included in this study.

DataData

• RLR sea level data from PSMSL (1023 stations)• GIA corrections from Peltier (2001)• SLP corrections • 12 regions

Global sea level (GSL) reconstruction (1807-2003)Global sea level (GSL) reconstruction (1807-2003)

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Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Virtual station spatial stackingVirtual station spatial stacking

height = 14

wpacific

Individual tide gauge records

Regional average

Binomial tree to illustrate the ‘virtual station’ stacking method. Top-node represents the regional average, bottom nodes the tide gauge records, and rest of nodes are virtual stations.

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Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Jevrejeva et al., Jevrejeva et al., Nonlinear trends and multi-year cycle in sea level records. Nonlinear trends and multi-year cycle in sea level records. Journal of Journal of Geophysical ResearchGeophysical Research, 111, 2005JC003229, 2006, 111, 2005JC003229, 2006. . Data: Data: www.pol.ac.uk/psmsl/author_archive/jevrejeva_et_al._jgr.htmlwww.pol.ac.uk/psmsl/author_archive/jevrejeva_et_al._jgr.html

Global sea level (GSL) reconstruction (1807-Global sea level (GSL) reconstruction (1807-2003)2003)

Page 13: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

Eruptions causing the largest radiative forcing Eruptions causing the largest radiative forcing since 1890since 1890

5 largest eruptions have been modelled

to have an impact on sea

level.

We focus on these.

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Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

ResultsResults

Sea level surrounding 5 major volcanic eruptions and the average sea level in these 5 periods. The

solid black curve shows detrended GSL (grey shows 95% confidence interval). Boxes show the median

sea level (centre line of box) of the “Before”, “Rise” and “Drop” windows. Top and bottom edges show

the 95% confidence interval of the median.

Average impact of 5 major volcanoes on detrended GSL as observed in tide gauge records (solid black curve). Coloured lines show detrended GSL around

the individual eruptions.

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How robust is the result?How robust is the result?

Average impact of 4 major volcanoes (excluding the 1902 Santa Maria eruption) on sea level. Boxes show the median sea level (centre line of box) of the “Before”, “Rise”

and “Drop” windows. Top and bottom edges show the 95% confidence interval of the

median.

Average impact of 9 major volcanoes on sea level weighted by global average

stratospheric optical depth. Boxes show the mean sea level (centre line of box) of the “Before”, “Rise” and “Drop” windows with top and bottom edges showing the 95%

confidence interval of the window mean. Thin green line shows detrended GSL, but weighted by Southern Hemisphere

stratospheric aerosol optical depth.

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Difference between modeled and observed effectDifference between modeled and observed effect

Church et al., 2005

Modeled sea level Observed sea level

Grinsted et al., 2007

Page 17: Observational evidence for volcanic impact on sea level and the global water cycle

Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008Grinsted et al., Volcanic impact on sea level and the water cycle, EGU 2008

SummarySummary

• We examine the average impact on observed GSL of the 5 volcanic eruptions with the largest stratospheric aerosol loading since 1890

• We find that the initial response to a volcanic eruption is a significant rise in sea level of 9±3 mm in the first year after the eruption

• This is followed by a drop of 7±3 mm in the period 2-3 years after the eruption relative to pre-eruption sea level.

• We suggest that the mechanism is a transient disturbance of the water cycle with a delayed response of land river runoff relative to ocean evaporation and global precipitation that affects global sea level.

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ReferenceReference

Grinsted, A., J.C. Moore, and S. Jevrejeva. 2007. Observational evidence for volcanic impact on sea level and the global water cycle, PNAS, Vol, 104, nr. 50, 19730-19734,

www.pnas.org_cgi_doi_10.1073_pnas.0705825104