Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models

This paper summarises the crossover adjustment of approximately 90,000-line-km of ship-track gravity observations around New Zealand. The adjustment reduced the standard deviation of the ~106 crossovers from ~2.0 mgal to ~0.3 mgal. These data were then used to assess four different grids of satellit...

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Main Authors: Amos, Matthew, Featherstone, Will, Brett, J.
Other Authors: Christopher Jekeli
Format: Conference Paper
Published: Springer 2005
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/20408
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author Amos, Matthew
Featherstone, Will
Brett, J.
author2 Christopher Jekeli
author_facet Christopher Jekeli
Amos, Matthew
Featherstone, Will
Brett, J.
author_sort Amos, Matthew
building Curtin Institutional Repository
collection Online Access
description This paper summarises the crossover adjustment of approximately 90,000-line-km of ship-track gravity observations around New Zealand. The adjustment reduced the standard deviation of the ~106 crossovers from ~2.0 mgal to ~0.3 mgal. These data were then used to assess four different grids of satellite-altimeter-derived gravity anomalies. The KMS02 altimeter grid was selected for use around New Zealand as it gave a better fit to the coastal ship-track data. Least-squares collocation was then used to 'drape' the altimetry onto the crossover-adjusted ship-tracks to counter the well-known problems with satellite altimeter data near the coast. The precision of this merged ship-altimeter gravity dataset is estimated to be 3.5 mgal.
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spelling curtin-20.500.11937-204082022-10-20T04:47:14Z Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models Amos, Matthew Featherstone, Will Brett, J. Christopher Jekeli Luisa Bastos Joana Fernandes crossover adjustment satellite altimetry geopotential model marine gravimetry gravity This paper summarises the crossover adjustment of approximately 90,000-line-km of ship-track gravity observations around New Zealand. The adjustment reduced the standard deviation of the ~106 crossovers from ~2.0 mgal to ~0.3 mgal. These data were then used to assess four different grids of satellite-altimeter-derived gravity anomalies. The KMS02 altimeter grid was selected for use around New Zealand as it gave a better fit to the coastal ship-track data. Least-squares collocation was then used to 'drape' the altimetry onto the crossover-adjusted ship-tracks to counter the well-known problems with satellite altimeter data near the coast. The precision of this merged ship-altimeter gravity dataset is estimated to be 3.5 mgal. 2005 Conference Paper http://hdl.handle.net/20.500.11937/20408 10.1007/3-540-26932-0_46 Springer restricted
spellingShingle crossover adjustment
satellite altimetry
geopotential model
marine gravimetry
gravity
Amos, Matthew
Featherstone, Will
Brett, J.
Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models
title Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models
title_full Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models
title_fullStr Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models
title_full_unstemmed Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models
title_short Crossover Adjustment of New Zealand Marine Gravity Data, and Comparisons with Satellite Altimetry and Global Geopotential Models
title_sort crossover adjustment of new zealand marine gravity data, and comparisons with satellite altimetry and global geopotential models
topic crossover adjustment
satellite altimetry
geopotential model
marine gravimetry
gravity
url http://hdl.handle.net/20.500.11937/20408