KenMankoff

The role of Pine Island Glacier ice shelf basal channels in deep-water upwelling, polynyas and ocean circulation in Pine Island Bay, Antarctica

The role of Pine Island Glacier ice shelf basal channels in deep-water upwelling, polynyas and ocean circulation in Pine Island Bay, Antarctica

@article{Mankoff:2012The-role,
	Title = {{The role of Pine Island Glacier ice shelf basal
                  channels in deep water upwelling, polynyas, and
                  ocean circulation in Pine Island Bay, Antarctica}},
	Author = {Kenneth D. Mankoff and Stanley S. Jacobs and
                  Slawek M. Tulaczyk and Sharon E. Stammerjohn},
	Journal = {Annals of Glaciology},
	Number = {60},
	Volume = {53},
	Year = {2012},
        DOI = {10.3189/2012AoG60A062}}

Pine Island Glacier and Pine Island Bay

Pine Island Glacier and Pine Island Bay

Pine Island Bay in the southeast Amundsen Sea, Antarctica, on 16 Nov 2008. Upwelling, melt-laden outflow plumes emerge from beneath the adjacent Pine Island Glacier ice shelf (top center) and mix in the bay waters. Warm red colors show sea surface temperatures more than a degree warmer than the near-freezing dark blue color. Cyclonic circulation in the bay is framed by the ice shelf, land ice and sea ice, in gray-scale with the darker shades colder. Landsat Enhanced Thematic Mapper Plus image, thermal infrared (channel 6H), subset of scene #LE72331132008321EDC00.

@article{Mankoff:2012The-role,
	Title = {{The role of Pine Island Glacier ice shelf basal
                  channels in deep water upwelling, polynyas, and
                  ocean circulation in Pine Island Bay, Antarctica}},
	Author = {Kenneth D. Mankoff and Stanley S. Jacobs and
                  Slawek M. Tulaczyk and Sharon E. Stammerjohn},
	Journal = {Annals of Glaciology},
	Number = {60},
	Volume = {53},
	Year = {2012},
        DOI = {10.3189/2012AoG60A062}}

Kinects as sensors in earth science: glaciological, geomorphological, and hydrological applications

Last week I presented a poster at the 2011 AGU Fall Meeting. It has generated some press thanks to an article in Wired. If you are interested in the poster it is available by clicking on the image below.

AGU Poster: `Kinects as sensors in earth science: glaciological, geomorphological, and hydrological applications`

@conference{Mankoff:2011Kinects,
  Author = {Kenneth D. Mankoff and Tess Alethea Russo and
            Benjamin Kenneth Norris and Saffia Hossainzadeh and
            Lucas H. Beem and Jacob I. Walter and
            Slawek M. Tulaczyk},
  Title = {{Kinects as sensors in earth science: glaciological,
            geomorphological, and hydrological applications}},
  Address = {San Francisco, CA},
  Booktitle = {American Geophysical Union, Fall Meeting},
  Month = {December 5 - 9,},
  Note = {Abstract \#C41D-0442.},
  Year = {2011}}

Pine Island Glacier Publication TimeMap

In which I present a rough geo-spatial-temporal map of Pine Island Glacier (PIG) publications.

Geo-spatial-temporal time-map of Pine Island Glacier (PIG) publications

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ANDRILL in Google Earth

I’ve released my Google Earth layer. Your comments and suggestions and data are welcome.

The KML (download here) is a very small network access file. Load it once, save it in the Google Earth sidebar, and all updates will be available each time you launch Google Earth. You need the latest Google Earth to view this layer.

This was presented at the SCAR IASC conference in St. Petersburg, Russia, July 8-11, 2008.

@conference{Mankoff:2008SCAR,
        Author = {K. D. Mankoff and the SMS Project Science Team},
        Title = {{An ANDRILL SMS ARISE Educational Software Package:
                From a microscope in Antarctica 20 million years ago
                to a global overview 100 years in the future}},
        Organization = {SCAR / IASC Open Science Conference},
        Address = {St. Petersburg, Russia},
        Month = {July 8-11},
        Year = {2008},
        Abstract = {We present an education software product
                (Google Earth Layer) that allows exploration of the
                ANDRILL SMS project. The geospatial, micro-to-macro,
                and multi-layering capabilities of Google Earth are
                used to allow viewers to tie together concepts from a
                microscopic view to a global overview. The journey
                begins with a microscopic view of diatoms in a
                borehole under the sea under the ice in Antarctica,
                and ends with a global overview of what the climate
                might look like in the year 2100 as calculated by the
                GISS Model II GCM from EdGCM. Paleo, present,
                and future GCM scenarios are available for users to
                explore more on their own using EdGCM.}}