grace. see movie free air gravity anomalies derived from radar altimetric determinations of geoid...

9
GRACE

Upload: dion-stocking

Post on 16-Dec-2015

215 views

Category:

Documents


2 download

TRANSCRIPT

Page 1: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

GRACE

Page 2: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

See movie

Page 3: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

Free air gravity anomalies derived from radar altimetric determinations of geoid height

milligals

Page 4: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

Bathymetry determined from satellite radar derived gravity plus shipboard measurements

Page 5: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

Major types of isostatic compensation

1. Airy: crustal root compensates elevated topographya. Ocean-continent crustal thicknessesb. Majority of variations in elevations on continental

mountain beltsc. Oceanic plateaus

2. Thermal: elevated topography a result of thermal expansiona. Ocean ridge systemb. Basin and Range

3. Flexural isostasya. Bending of the lithosphere: oceanic trenchesb. Regional isostasy

Page 6: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

crust

mantle

Airy isostasy

crustal thickening

Page 7: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

crust

mantle

Airy isostasy

topographic “load”

compensating root

Simple Airy isostasy is dealt with in more detail ingrav_anom.ppt

Page 8: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

crust

mantle lithosphere

mantle athenosphere

1300 C

Temperature, degrees C

0 1300

50

100

150

200

Thermal isostasy

A

B

Lithospheric

thinning

uplift from thermal expansion

A

B

Thermal thinning and uplift are dealt with in more detail inthermal.pdf

Page 9: GRACE. See movie Free air gravity anomalies derived from radar altimetric determinations of geoid height milligals

Outstanding continental examples of thermal or Airy isostasy

thermal

AiryAiry