Examples from the Mississippi Delta and Greenland · Role of High-Precision GPS in Flood Hazard and...

Role of High-Precision GPS

in Flood Hazard and Sea

Level Rise Studies

Examples from the Mississippi Delta and

Greenland

Tim Dixon University of South Florida

COPYRIGHT - Tele-Rilevamento Europa 2005

Flood Hazard Background

Coastal flooding and coastal land loss reflect

combined effects of land subsidence and sea

level rise (SLR)

For next few decades, SLR is insignificant (3

mm/yr x 30 yrs = 9 cm) but subsidence effects

can be large (20 mm/yr x 30 yrs = 60 cm)

Example: New Orleans and Mississippi Delta –

high land subsidence rates

On longer time scales, SLR will become

significant

Greenland likely to be significant contributor to

SLR over next 100 years

Cost of Hazards

US Domestic, insured + uninsured

(most are flood-related)

Source:

Munich Re

What causes low elevation and flooding in

New Orleans?

• Subsidence: combination of effects, exacerbated by anthropogenic intervention in natural system

• All deltas subside, but natural sedimentation patterns replenish topmost layer, maintaining height near sea level; Levees restrict natural sedimentation

• Would be useful to know quantitative contributions of various subsidence processes

• Measuring spatial patterns of subsidence can help distinguish causes

Causes of subsidence

• Sediment loading

• Sediment compaction,

dessication, oxidation

• Fluid withdrawal:

(water; oil and gas

production)

Main Cause of Low Elevation in New Orleans

• Oxidation & sediment compaction – exponential

processes

• Some parts of city currently lie >3 m below sea level

• Assume they were at or near sea level before

construction of levees

and marsh drainage

(~1860 AD) began

process of oxidation,

sediment compaction.

Sub rates

>20 mm/yr

Sub rates

few mm/yr

(today)

Active Tectonics May Also Play a Role

Dokka, Sella and Dixon (2006)

*Mississippi Delta slides on several listric

normal faults towards Gulf of Mexico

*Weak salt layer acts as decollement

*Mainly horizontal motion

Geomorphic

Boundary

Causes of Delta Subsidence

• Unlike New Orleans, oxidation should

not be significant

• Compaction of Holocene sediments

(1-2 mm/yr?)

• Mass loading of delta (Ivins et al.

2007) (3-6 mm/yr) predicts simple

pattern observed

Ivins, Dokka

& Blom, 2007

Causes of Horizontal Motion

• Southward motion at ~0.5 mm/yr reflects

sliding of Miss. Delta block on deep, salt-

related decollement

• Recent & Holocene mass loading of delta

may play a role

• Growth normal faults are active

GRACE Results, 2002-2011

Importance of Glacial Isostatic Adjustment

• GIA reflects long term response of

mantle to crustal unloading after Last

Glacial Maximum (LGM) ~ 20,000 years

• GRACE sensitive to GIA model

• GIA models depend on:

– Mantle viscosity structure (poorly known)

– Ice melting history (very poorly known)

What is relation of GIA to present uplift

signal from anthropogenic warming? • In principle, can use isostasy to infer ice

melting rate (loss of Greenland ice results in

uplift)

• Problems

impact of past events is significant (visco-elastic

response from LGM)

mantle viscosity limit present-day response

• GIA is both a potential tool for ice melt studies,

and a noise source

• GPS can help constrain GIA, and measure

present mass loss directly

•Glacial Isostatic Adjustment in

North America observed with GPS

•Shows long term response to

melting since LGM

UPLIFT

SUBSIDENCE

1995 2000 2005 2010−4000

−3000

−2000

−1000

Time (Year)

1995 2000 2005 20100

Time (Year)

Cumulative changes in the mass of GrIS (Sheperd et al., 2012)

Time series of GPS vertical component position estimates for Greenland

a = 0.6 +/- 0.1 mm/yr/yr

a = -23.2 +/- 0.5 Gt/yr/yr

Model (red curve):

Initial Velocity

Constant acceleration

Annual & semi-

annual terms

Zero Mean

Annual Signal

Elastic response implies uplift

sensitive to seasonal melting

Can be used to compare annual variations,

investigate details of acceleration at

individual sites

Losses occur during short summer melt

season

Duration of summer

melt season

Amount of

summer

uplift

Time (Year)

ical D

Timing of accelerated

uplift from a GIA-GPS

Model: mid-late 1990’s,

a time when many

changes were happening

in North Atlantic ocean

circulation

Summary

• High precision GPS can monitor geologic and

anthropogenic deformation processes in Gulf coast,

and details of Greenland melting

• 1-2 mm precision in vertical component

• Subsidence of Miss. Delta and New Orleans levees

continues, increasing future flood potential

• Subsidence “budget” still unclear (what are various

sources?)

• Miss. Delta moves south at ~0.5 mm/yr, probably

related to listric faults that exploit ductile salt at depth

• Greenland melting is accelerating. Now contributes ~ 1

mm/yr to global sea level rise budget.

Examples from the Mississippi Delta and Greenland · Role of High-Precision GPS in Flood Hazard and...

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