New Zealand's dynamic deformation field
Database
Interferometric Synthetic Aperture Radar (InSAR) data provides a method to measure the deformation of the Earth's surface at high spatial resolutions over large areas. InSAR and GNSS data from 2003 to 2011 were used to measure nationwide surface velocities. Data in this file are from a Geophysical Research Letter publication.
Overview
Data include the full InSAR velocities, standalone GNSS over the same period and coastal Vertical Land Movement as detailed in the manuscript.
Publication: Hamling, I. J., Wright, T. J., Hreinsdóttir, S., & Wallace, L. M. (2022)(external link). A snapshot of New Zealand's dynamic deformation field from Envisat InSAR and GNSS observations between 2003 and 2011. Geophysical Research Letters, 49, e2021GL096465.
Cite as: GNS Science. (2021). A snapshot of New Zealand's dynamic deformation field from Envisat InSAR and GNSS observations between 2003 and 2011 [Data set]. GNS Science. https://doi.org/10.21420/E1C1-MQ19
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Locations
- Te Tai-o-Aorere / Tasman
- Rangitāhua / Kermadec Islands
- Rēkohu / Chatham Islands
- Rakiura / Stewart Island
- Murihiku / Southland
- Ōtepoti / Dunedin
- Ōtākou / Otago
- Ōtautahi / Christchurch
- Waitaha / Canterbury
- Kaikōura
- Te Tai Poutini / West Coast
- Te Tauihu-o-te-waka/ Marlborough
- Whakatū / Nelson
- Antarctica
- Te Whanga-nui-a-Tara / Wellington
- Manawatū-Whanganui
- Central Plateau
- Taranaki
- Te Matau-a-Māui / Hawke's Bay
- Te Tai Rāwhiti / Gisborne
- Te Moana-a-Toi / Bay of Plenty
- Waikato
- Tāmaki Makaurau / Auckland
- Te Tai Tokerau / Northland
- Aotearoa / New Zealand
- Pacific Islands