Comment on tc-2021-8 Article Swipe
Alexandra L. Post
,
Emrys Phillips
,
Chris Carson
,
J. A. Smith
·
YOU?
·
· 2021
· Open Access
·
· DOI: https://doi.org/10.5194/tc-2021-8-rc2
YOU?
·
· 2021
· Open Access
·
· DOI: https://doi.org/10.5194/tc-2021-8-rc2
Understanding past retreat of Antarctic ice margins provides valuable insight for predicting how ice sheets may respond to future environmental change. This study, based on high resolution multibeam bathymetry from the nearshore region of the Windmill Islands, East Antarctica, reveals a style of retreat that has been rarely observed on the Antarctic margin. A suite of seafloor features record the final retreat stages of a relatively thin, and increasingly fractured tidewater glacier confined within narrow troughs and embayments, forming a suite of features more typical of warm-based ice, but occurring here in a region of cold-based ice with limited surface meltwater production. The pattern of moraines and crevasse squeeze ridges, reveals strong topographic and substrate control on the nature of ice sheet retreat. Topographic control is indicated by fine-scale variability in the orientation and distribution of glacial landforms, which show that the seabed topography influenced the shape of the ice margin, caused deflection of ice flow and led to the separation of flow downstream from topographic highs. The availability of water saturated marine sediments within the troughs and depressions also had a profound effect on the landform record, facilitating the construction of moraines and crevasse squeeze ridges within topographic lows, corresponding to areas of modern sediment accumulation. Surrounding areas of crystalline bedrock, by contrast, acted as sticky spots and lack a well-developed landform record. This seafloor glacial record emphasises the importance of understanding the bed topography and substrate when predicting the nature of ice margin retreat and provides new perspectives for understanding the stability of the East Antarctic margin.
Related Topics
Concepts
Geology
Landform
Moraine
Glacier
Geomorphology
Seabed gouging by ice
Ice sheet
Ice stream
Bedrock
Ice divide
Crevasse
Meltwater
Ice shelf
Paleontology
Oceanography
Cryosphere
Sea ice
Metadata
- Type
- peer-review
- Language
- en
- Landing Page
- https://doi.org/10.5194/tc-2021-8-rc2
- OA Status
- gold
- References
- 45
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4256688250
All OpenAlex metadata
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https://openalex.org/W4256688250Canonical identifier for this work in OpenAlex
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https://doi.org/10.5194/tc-2021-8-rc2Digital Object Identifier
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Comment on tc-2021-8Work title
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peer-reviewOpenAlex work type
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enPrimary language
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2021Year of publication
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2021-05-13Full publication date if available
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Alexandra L. Post, Emrys Phillips, Chris Carson, J. A. SmithList of authors in order
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-
https://doi.org/10.5194/tc-2021-8-rc2Publisher landing page
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YesWhether a free full text is available
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goldOpen access status per OpenAlex
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https://doi.org/10.5194/tc-2021-8-rc2Direct OA link when available
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Geology, Landform, Moraine, Glacier, Geomorphology, Seabed gouging by ice, Ice sheet, Ice stream, Bedrock, Ice divide, Crevasse, Meltwater, Ice shelf, Paleontology, Oceanography, Cryosphere, Sea iceTop concepts (fields/topics) attached by OpenAlex
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0Total citation count in OpenAlex
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| abstract_inverted_index.ice | 5, 13, 96, 120, 149, 154, 243 |
| abstract_inverted_index.led | 157 |
| abstract_inverted_index.may | 15 |
| abstract_inverted_index.new | 248 |
| abstract_inverted_index.the | 30, 34, 50, 59, 117, 131, 141, 145, 148, 159, 175, 185, 189, 229, 233, 240, 252, 255 |
| abstract_inverted_index.East | 37, 256 |
| abstract_inverted_index.This | 21, 224 |
| abstract_inverted_index.also | 179 |
| abstract_inverted_index.been | 46 |
| abstract_inverted_index.flow | 155, 162 |
| abstract_inverted_index.from | 29, 164 |
| abstract_inverted_index.here | 90 |
| abstract_inverted_index.high | 25 |
| abstract_inverted_index.ice, | 87 |
| abstract_inverted_index.lack | 219 |
| abstract_inverted_index.more | 83 |
| abstract_inverted_index.past | 1 |
| abstract_inverted_index.show | 139 |
| abstract_inverted_index.that | 44, 140 |
| abstract_inverted_index.when | 238 |
| abstract_inverted_index.with | 97 |
| abstract_inverted_index.acted | 214 |
| abstract_inverted_index.areas | 202, 208 |
| abstract_inverted_index.based | 23 |
| abstract_inverted_index.final | 60 |
| abstract_inverted_index.lows, | 199 |
| abstract_inverted_index.shape | 146 |
| abstract_inverted_index.sheet | 121 |
| abstract_inverted_index.spots | 217 |
| abstract_inverted_index.style | 41 |
| abstract_inverted_index.suite | 54, 80 |
| abstract_inverted_index.thin, | 66 |
| abstract_inverted_index.water | 170 |
| abstract_inverted_index.which | 138 |
| abstract_inverted_index.caused | 151 |
| abstract_inverted_index.effect | 183 |
| abstract_inverted_index.future | 18 |
| abstract_inverted_index.highs. | 166 |
| abstract_inverted_index.margin | 244 |
| abstract_inverted_index.marine | 172 |
| abstract_inverted_index.modern | 204 |
| abstract_inverted_index.narrow | 74 |
| abstract_inverted_index.nature | 118, 241 |
| abstract_inverted_index.rarely | 47 |
| abstract_inverted_index.record | 58, 227 |
| abstract_inverted_index.region | 32, 93 |
| abstract_inverted_index.ridges | 196 |
| abstract_inverted_index.seabed | 142 |
| abstract_inverted_index.sheets | 14 |
| abstract_inverted_index.stages | 62 |
| abstract_inverted_index.sticky | 216 |
| abstract_inverted_index.strong | 111 |
| abstract_inverted_index.study, | 22 |
| abstract_inverted_index.within | 73, 174, 197 |
| abstract_inverted_index.change. | 20 |
| abstract_inverted_index.control | 115, 124 |
| abstract_inverted_index.forming | 78 |
| abstract_inverted_index.glacial | 136, 226 |
| abstract_inverted_index.glacier | 71 |
| abstract_inverted_index.insight | 9 |
| abstract_inverted_index.limited | 98 |
| abstract_inverted_index.margin, | 150 |
| abstract_inverted_index.margin. | 52, 258 |
| abstract_inverted_index.margins | 6 |
| abstract_inverted_index.pattern | 103 |
| abstract_inverted_index.record, | 187 |
| abstract_inverted_index.record. | 223 |
| abstract_inverted_index.respond | 16 |
| abstract_inverted_index.retreat | 2, 43, 61, 245 |
| abstract_inverted_index.reveals | 39, 110 |
| abstract_inverted_index.ridges, | 109 |
| abstract_inverted_index.squeeze | 108, 195 |
| abstract_inverted_index.surface | 99 |
| abstract_inverted_index.troughs | 75, 176 |
| abstract_inverted_index.typical | 84 |
| abstract_inverted_index.Islands, | 36 |
| abstract_inverted_index.Windmill | 35 |
| abstract_inverted_index.bedrock, | 211 |
| abstract_inverted_index.confined | 72 |
| abstract_inverted_index.crevasse | 107, 194 |
| abstract_inverted_index.features | 57, 82 |
| abstract_inverted_index.landform | 186, 222 |
| abstract_inverted_index.moraines | 105, 192 |
| abstract_inverted_index.observed | 48 |
| abstract_inverted_index.profound | 182 |
| abstract_inverted_index.provides | 7, 247 |
| abstract_inverted_index.retreat. | 122 |
| abstract_inverted_index.seafloor | 56, 225 |
| abstract_inverted_index.sediment | 205 |
| abstract_inverted_index.valuable | 8 |
| abstract_inverted_index.Antarctic | 4, 51, 257 |
| abstract_inverted_index.contrast, | 213 |
| abstract_inverted_index.fractured | 69 |
| abstract_inverted_index.indicated | 126 |
| abstract_inverted_index.meltwater | 100 |
| abstract_inverted_index.multibeam | 27 |
| abstract_inverted_index.nearshore | 31 |
| abstract_inverted_index.occurring | 89 |
| abstract_inverted_index.saturated | 171 |
| abstract_inverted_index.sediments | 173 |
| abstract_inverted_index.stability | 253 |
| abstract_inverted_index.substrate | 114, 237 |
| abstract_inverted_index.tidewater | 70 |
| abstract_inverted_index.bathymetry | 28 |
| abstract_inverted_index.cold-based | 95 |
| abstract_inverted_index.deflection | 152 |
| abstract_inverted_index.downstream | 163 |
| abstract_inverted_index.emphasises | 228 |
| abstract_inverted_index.fine-scale | 128 |
| abstract_inverted_index.importance | 230 |
| abstract_inverted_index.influenced | 144 |
| abstract_inverted_index.landforms, | 137 |
| abstract_inverted_index.predicting | 11, 239 |
| abstract_inverted_index.relatively | 65 |
| abstract_inverted_index.resolution | 26 |
| abstract_inverted_index.separation | 160 |
| abstract_inverted_index.topography | 143, 235 |
| abstract_inverted_index.warm-based | 86 |
| abstract_inverted_index.Antarctica, | 38 |
| abstract_inverted_index.Surrounding | 207 |
| abstract_inverted_index.Topographic | 123 |
| abstract_inverted_index.crystalline | 210 |
| abstract_inverted_index.depressions | 178 |
| abstract_inverted_index.embayments, | 77 |
| abstract_inverted_index.orientation | 132 |
| abstract_inverted_index.production. | 101 |
| abstract_inverted_index.topographic | 112, 165, 198 |
| abstract_inverted_index.variability | 129 |
| abstract_inverted_index.availability | 168 |
| abstract_inverted_index.construction | 190 |
| abstract_inverted_index.distribution | 134 |
| abstract_inverted_index.facilitating | 188 |
| abstract_inverted_index.increasingly | 68 |
| abstract_inverted_index.perspectives | 249 |
| abstract_inverted_index.Understanding | 0 |
| abstract_inverted_index.accumulation. | 206 |
| abstract_inverted_index.corresponding | 200 |
| abstract_inverted_index.environmental | 19 |
| abstract_inverted_index.understanding | 232, 251 |
| abstract_inverted_index.well-developed | 221 |
| cited_by_percentile_year | |
| corresponding_author_ids | https://openalex.org/A5044436404, https://openalex.org/A5051189061 |
| countries_distinct_count | 2 |
| institutions_distinct_count | 4 |
| corresponding_institution_ids | https://openalex.org/I1331816111 |
| sustainable_development_goals[0].id | https://metadata.un.org/sdg/14 |
| sustainable_development_goals[0].score | 0.8600000143051147 |
| sustainable_development_goals[0].display_name | Life below water |
| citation_normalized_percentile |