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 [[https://cosmognosis.wordpress.com/2021/01/25/antarctic-deglaciation-in-one-figure/|Antarctic deglaciation in one figure]]: a blog posting by Greg Balco that summarizes Holocene exposure-age data from Antarctica to highlight the fact that nearly all LGM-to-present ice sheet thinning in Antarctica appears to have taken place in only a few thousand years in the early to middle Holocene. [[https://cosmognosis.wordpress.com/2021/01/25/antarctic-deglaciation-in-one-figure/|Antarctic deglaciation in one figure]]: a blog posting by Greg Balco that summarizes Holocene exposure-age data from Antarctica to highlight the fact that nearly all LGM-to-present ice sheet thinning in Antarctica appears to have taken place in only a few thousand years in the early to middle Holocene.
  
-[[https://pubs.geoscienceworld.org/gsa/geology/article/49/1/91/590796/Exposure-age-data-from-across-Antarctica-reveal|Nothing has happened in interior Antarctica since the mid-Miocene]]: a paper by Perry Spector that uses the ICE-D:ANTARCTICA database to show that the geomorphic record in interior Antarctica extends up to but not past the dramatic climate cooling that established the polar desert climate regime 14 million years ago. +[[https://www.sciencedirect.com/science/article/abs/pii/S0277379118307728|A paper by David Small and several others]] also makes use of an early version of the database to estimate past ice sheet thinning rates at various places in Antarctica. 
  
-[[https://cosmognosis.wordpress.com/2021/12/10/find-the-gap-the-late-holocene-exposure-age-gap-in-antarctica-that-is/|Find the Gap!]] A [[https://tc.copernicus.org/articles/16/1543/2022/tc-16-1543-2022.pdf|paper by Joanne Johnson and many others]] uses the ICE-D:ANTARCTICA database to explore evidence for Holocene retreat and readvance of Antarctic ice sheet grounding lines. See Figure 2 in the paper. There is more back story about the figure in a [[https://cosmognosis.wordpress.com/2021/12/10/find-the-gap-the-late-holocene-exposure-age-gap-in-antarctica-that-is|blog posting]].+[[https://pubs.geoscienceworld.org/gsa/geology/article/49/1/91/590796/Exposure-age-data-from-across-Antarctica-reveal|Almost nothing has happened in interior Antarctica since the mid-Miocene]]: a paper by Perry Spector that uses the ICE-D:ANTARCTICA database to show that the geomorphic record in interior Antarctica extends up to but not past the dramatic climate cooling that established the polar desert climate regime 14 million years ago.  
 + 
 +Find the Gap! A [[https://tc.copernicus.org/articles/16/1543/2022/tc-16-1543-2022.pdf|paper by Joanne Johnson and many others]] uses the ICE-D:ANTARCTICA database to explore evidence for Holocene retreat and readvance of Antarctic ice sheet grounding lines. See Figure 2 in the paper. There is more back story about the figure in a [[https://cosmognosis.wordpress.com/2021/12/10/find-the-gap-the-late-holocene-exposure-age-gap-in-antarctica-that-is|blog posting]]. 
 + 
 +[[https://www.nature.com/articles/s43017-022-00309-5|A synoptic view of Antarctic ice sheet change in the Holocene:]] A paper by Richard Jones and others in Nature Reviews uses the ICE-D database to understand the Antarctic contribution to Holocene sea level change.  
 + 
 +[[https://essd.copernicus.org/preprints/essd-2022-398/|Antarctic ice sheet model benchmarking:]] A paper by Benoit Lecavalier and others in Earth System Science Data uses the ICE-D:ANTARCTICA database as part of an observational constraint database intended for benchmarking LGM-to-present ice sheet model simulations. 
  
 === ICE-D:ALPINE === === ICE-D:ALPINE ===
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 [[https://drive.google.com/file/d/1jLp5TrBg12e8hoJshiWdU67K2FOZWz5j/view?usp=sharing|Spatio-temporal patterns of Late Pleistocene mountain glaciation in the western United States]]: A GSA presentation demonstrating the use of ICE-D Alpine for a simple analysis of terminal and recessional moraine exposure ages and corresponding ELAs in the conterminous western U.S.  [[https://drive.google.com/file/d/1jLp5TrBg12e8hoJshiWdU67K2FOZWz5j/view?usp=sharing|Spatio-temporal patterns of Late Pleistocene mountain glaciation in the western United States]]: A GSA presentation demonstrating the use of ICE-D Alpine for a simple analysis of terminal and recessional moraine exposure ages and corresponding ELAs in the conterminous western U.S. 
 +
 +[[https://www.annualreviews.org/doi/abs/10.1146/annurev-earth-081619-052609|A paper in Annual Reviews of Earth and Planetary Sciences]] uses the ICE-D:ALPINE database to show how one might learn about synoptic paleoclimate from large data sets of cosmogenic-nuclide exposure ages on alpine glacier moraines. 
  
 [[https://drive.google.com/file/d/1jOchX7EH1KzO5UxUASadf8EZh1BdO3HN/view?usp=sharing|Late Pleistocene mountain glacier equilibrium line altitudes in the Great Basin and neighboring settings in the southwestern U.S.A.]]: A GSA presentation demonstrating the combination of ICE-D Alpine exposure ages of moraines with a set of geospatial tools for 3D reconstructions of mountain glacier surfaces and ELAs.  [[https://drive.google.com/file/d/1jOchX7EH1KzO5UxUASadf8EZh1BdO3HN/view?usp=sharing|Late Pleistocene mountain glacier equilibrium line altitudes in the Great Basin and neighboring settings in the southwestern U.S.A.]]: A GSA presentation demonstrating the combination of ICE-D Alpine exposure ages of moraines with a set of geospatial tools for 3D reconstructions of mountain glacier surfaces and ELAs. 
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 [[https://crep.otelo.univ-lorraine.fr/|The CREp online exposure age calculator]]: CREp uses the ICE-D:CALIBRATION database to provide highly configurable production rate calibration data for exposure-dating applications.  [[https://crep.otelo.univ-lorraine.fr/|The CREp online exposure age calculator]]: CREp uses the ICE-D:CALIBRATION database to provide highly configurable production rate calibration data for exposure-dating applications. 
  
-==== Not so science applications ==== 
- 
-The ICE-D project has a [[https://twitter.com/ice_d_database|Twitter account]]. Randomly selected alpine glacier moraines on Wednesdays. Antarctic field photos on Fridays.