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Natalie Robinson
Antarctic, climate and atmospheric researcher

Natalie Robinson

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Antarctic, climate and atmospheric researcher
Work field
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Female
Natalie Robinson
The details (from wikipedia)

Biography

Natalie Robinson, an Antarctic researcher, is based at the National Institute of Water and Atmospheric Research in New Zealand. She led the final two K131 Science Events on the sea ice of McMurdo Sound, Antarctica.

Education

Robinson grew up in the Hawke's Bay Region and moved to Victoria University of Wellington to complete her MSc (2005) on tides beneath the McMurdo Ice Shelf with data collected during the ANDRILL project with Alex Pyne and Peter Barrett.She then completed her PhD (2012) at the University of Otago under the supervision of Pat Langhorne. She now works as a research scientist at National Institute of Water and Atmospheric Research.

Career and impact

Dr. Robinson has led a number of field expeditions to the sea ice of McMurdo Sound, Antarctica.In 2015 she was awarded a prestigious Marsden grant to study ice roughness beneath ice shelf affected sea ice. This resulted in two expeditions to McMurdo Sound.Her studies showed that new ice crystals could refreeze on the underside of sea ice and make the underside much rougher than under smooth melting ice.

This work used Antarctic infrastructure developed by Timothy Haskell. Robinson led the final expeditions using the "K131" Camp Haskell. The "K131" is an event designation assigned by Antarctica New Zealand.

She has worked with the artist Gabby O'Connor when O'Connor participated in Robinson's 2017 field expedition. This resulted in an exhibition at the Otago Museum in 2018.

Robinson is an active communicator on climate, science, Antarctica and combining field work and family commitments.

Shipping container on the McMurdo Sound sea ice. This is an oceanographic laboratory as part of K131 and has a hole in the floor through which the ocean is accessed.

She is on the Council of the New Zealand Association of Scientists.

The contents of this page are sourced from Wikipedia article. The contents are available under the CC BY-SA 4.0 license.
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