mass and volume contribution to twentieth-century global sea level rise

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Mass and Volume Contribution to Twentieth-century Global Sea Level Rise L. Miller & B. C. Douglas Nature vol. 428, 2004

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Mass and Volume Contribution to Twentieth-century Global Sea Level Rise. L. Miller & B. C. Douglas. Nature vol. 428, 2004. Could water world really happen?. Interaction of temperature change with environmental system. Greenland Ice Sheet 7m GSLR. Antarctic+ GLIS 80m GSLR. - PowerPoint PPT Presentation

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Page 1: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Mass and Volume Contribution to Twentieth-century Global

Sea Level Rise

L. Miller & B. C. Douglas

Nature vol. 428, 2004

Page 2: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Could water world really happen?

Interaction of temperature change with environmental system

Water held in glaciers and small ice caps!!

Greenland Ice Sheet7m GSLR

Antarctic+ GLIS80m GSLR

Page 3: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

But by how much ?

1. Volume Change (Total Steric Sea Level, TSSL)

2. Mass Change (Eustatic change)

Exchange of water with atmosphere and continents

Temperature and salinity variations

Page 4: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Gauge Data

Total Steric Changes +Eustatic Changes

Isostatic Changes

Page 5: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Dynamic Height

Depth difference between two surfaces of constant pressure and gravity.

It is derived from hydrographic data (T, S, P)Ocean General Circulation Models (OGCM)

Page 6: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Different Approaches

Yearly average trend 1993-98 (3.2 + 0.2 mm/yr)TSC (temperature) (0-500m) 1993-98 (3.1 + 0.4mm/yr)Residual sea level (0.2 + 0.2 mm/yr)

5 year data trend

Topex/ Poseidon data from 1993-2001 (Cabanes et al., 2001)

Page 7: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

*Global mean TSC (0-3000m) (0.5 + 0.05 mm/yr)*Pseudo global mean TSC using data of 25 gauge sites (1.4 + 0.2 mm/yr)*PSMSL record at 25 tide gauge sites (1.6+0.15 mm/yr)

*TSSL= 0.55 + 0.07 mm/yr*HSC 0.05 + 0.02 mm/yr

*470 + 170 km3/yr fresh water*Mass increase 1.35+0.5 mm/yr

(Antonov et al., 2002)

Page 8: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

3rd IPCC report (2001)

IPCC adopted best estimates = 1.5 + 0.5 mm/yr

TSC = 0.7 mm/yr

CG = 0.2-0.4 mm/yr

MC = -0.2-0.6 mm/yr

TWS = -1.1- 0.4 mm/yr Sum = -0.8 –2.2 mm/yrAvg = 0.7 mm/yr

0

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+

Page 9: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Comparison of hydrographic and tide gauge measured sea level change in the

Eastern Pacific

TSSL = 0.5 mm/yrGauge data = 2 mm/yr

Page 10: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Local comparison

a. 0.5 mm/yr

c. 0.9 mm/yrGauge data = 1.7 mm/yr

b. 0.3 mm/yr

Page 11: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Regional comparison in the Eastern N. Atlantic

TSSL = 0.2 mm/yr

Gauge data = 2.1 &

1.9 mm/yr

Page 12: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Regional comparison in the Western N. Atlantic

Gauge data =1.9 mm/yr

Cabanes etal., 20018 sites = 0.5 mm/yr1 site = 6.7 mm/yr (NA)Avg = 1.2 mm/yr

Page 13: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Conclusions

*Overall gauge data = 1.5- 2.0 mm/yr GSLR for 20th century

Hydrographic data = 0.5 mm/yr

Mass Increase due to freshening = 1.4 mm/yr

* Satellite data = 2.5 mm/yr (1993-2003) Decadal data !!

Page 14: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Ocean freshening, sea level rising, sea ice meltingP. Wadhams, W. Munk(GRL., Vol. 31, 2004)

Arctic Sea Ice melting = (625 + 125) Km3/yr

Antarctic Ice thickening = (90 + 3) Km3/yr

Volume of fresh water = (325 + 105) Km3/yr

GSLR = mass + volume 0.6 + 0.5 = 1.1 mm/yr

Page 15: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Thanks

Page 16: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise
Page 17: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Total steric sea level change

1.Thermosteric change (TC)

2. Halosteric change (SC)

Page 18: Mass and Volume Contribution to Twentieth-century Global Sea Level Rise

Mass and Volume

L. Miller & B. C. Douglas

Nature vol. 428 2004