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
Abstract. New Zealand, unlike most countries, does not have a single national vertical datum. In-ste...
Sea surface gradients derived from the Geosat and ERS-1 satellite altimetry geodetic missions were i...
Marine gravity anomalies over the area 82°S, to 82°N and 0°E to 360°E on a 2′ × 2′ grid have been de...
Abstract. This paper summarises the crossover adjustment of approximately 90,000-line-km of ship-tra...
Abstract. This paper summarises the crossover adjustment of approximately 90,000-line-km of ship-tra...
© 2017 The Royal Society of New Zealand. We present 1 arc-minute Bouguer, Faye, free air and topogra...
We present 1 arc-minute Bouguer, Faye, free air and topography corrected gravity anomaly grids ...
The GMGA97, KMS01 and Sandwell's v.9.2 grids of marine gravity anomalies, derived from multi-mission...
v.9.2 grids of marine gravity anomalies, derived from multi-mission satellite altimetry, are compare...
This study compares global geopotential models (GGMs) released between 1996 and 2002, including four...
Satellite altimetry in near-coastal marine areas is notoriously problematic, and gravity anomalies d...
Abstract. New Zealand, unlike most countries, does not have a single national vertical datum. In-ste...
New Zealand, unlike most countries, does not have a single national vertical datum. Instead, twelve ...
Abstract. In order to create high-resolution gravity maps in oceanic areas, all type of data have to...
This study compares global geopotential models released between 1996 and 2002, including four that i...
Abstract. New Zealand, unlike most countries, does not have a single national vertical datum. In-ste...
Sea surface gradients derived from the Geosat and ERS-1 satellite altimetry geodetic missions were i...
Marine gravity anomalies over the area 82°S, to 82°N and 0°E to 360°E on a 2′ × 2′ grid have been de...
Abstract. This paper summarises the crossover adjustment of approximately 90,000-line-km of ship-tra...
Abstract. This paper summarises the crossover adjustment of approximately 90,000-line-km of ship-tra...
© 2017 The Royal Society of New Zealand. We present 1 arc-minute Bouguer, Faye, free air and topogra...
We present 1 arc-minute Bouguer, Faye, free air and topography corrected gravity anomaly grids ...
The GMGA97, KMS01 and Sandwell's v.9.2 grids of marine gravity anomalies, derived from multi-mission...
v.9.2 grids of marine gravity anomalies, derived from multi-mission satellite altimetry, are compare...
This study compares global geopotential models (GGMs) released between 1996 and 2002, including four...
Satellite altimetry in near-coastal marine areas is notoriously problematic, and gravity anomalies d...
Abstract. New Zealand, unlike most countries, does not have a single national vertical datum. In-ste...
New Zealand, unlike most countries, does not have a single national vertical datum. Instead, twelve ...
Abstract. In order to create high-resolution gravity maps in oceanic areas, all type of data have to...
This study compares global geopotential models released between 1996 and 2002, including four that i...
Abstract. New Zealand, unlike most countries, does not have a single national vertical datum. In-ste...
Sea surface gradients derived from the Geosat and ERS-1 satellite altimetry geodetic missions were i...
Marine gravity anomalies over the area 82°S, to 82°N and 0°E to 360°E on a 2′ × 2′ grid have been de...