Sea ice conditions within the Antarctic Marginal Ice Zone in summer 2016, onboard the SA Agulhas II
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| Autori principali: | , , , , , , |
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2018
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| _version_ | 1867170080784121856 |
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| author | de Jong, Ehlke Vichi, Marcello Saunders, Clinton F W Kotilainen, Mikko J Luyt, Hermann Peel, Stephen P M Swart, Daniël J |
| author_facet | de Jong, Ehlke Vichi, Marcello Saunders, Clinton F W Kotilainen, Mikko J Luyt, Hermann Peel, Stephen P M Swart, Daniël J |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Our knowledge of sea ice variability, which contributes to the detection of the Antarctic climate change trends, stems primarily from remotely sensed information. However, sea ice in the Southern Ocean is characterized by large variability that remains unresolved and limits our confidence on the remotely sensed products. Therefore, the in situ sea ice observations presented (according to the ASPeCt protocol) provide a greater understanding of the Antarctic sea ice environment - on a local scale - and allows us to evaluate remotely sensed products. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_885208 |
| institution | PANGAEA |
| language | en |
| publishDate | 2018 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Sea ice conditions within the Antarctic Marginal Ice Zone in summer 2016, onboard the SA Agulhas II de Jong, Ehlke Vichi, Marcello Saunders, Clinton F W Kotilainen, Mikko J Luyt, Hermann Peel, Stephen P M Swart, Daniël J AGULII201612; AGULII20161207_10; AGULII20161207_11; AGULII20161207_12; AGULII20161207_13; AGULII20161207_14; AGULII20161207_15; AGULII20161207_16; AGULII20161207_17; AGULII20161207_18; AGULII20161207_19; AGULII20161207_20; AGULII20161207_21; AGULII20161207_22; AGULII20161207_23; AGULII20161207_9; AGULII20161208_0; AGULII20161208_1; AGULII20161208_10; AGULII20161208_11; AGULII20161208_12; AGULII20161208_13; AGULII20161208_14; AGULII20161208_15; AGULII20161208_16; AGULII20161208_17; AGULII20161208_18; AGULII20161208_2; AGULII20161208_3; AGULII20161208_4; AGULII20161208_5; AGULII20161208_6; AGULII20161208_7; AGULII20161208_8; AGULII20161208_9; AGULII20161210_0; AGULII20161210_1; AGULII20161210_10; AGULII20161210_11; AGULII20161210_12; AGULII20161210_13; AGULII20161210_14; AGULII20161210_15; AGULII20161210_16; AGULII20161210_17; AGULII20161210_2; AGULII20161210_3; AGULII20161210_4; AGULII20161210_5; AGULII20161210_6; AGULII20161210_7; AGULII20161210_8; AGULII20161210_9; Comment; Comment of event; DATE/TIME; Event label; Floe size; Ice concentration; ICESUR; Ice survey; Ice type; Latitude of event; Lazarev Sea; Longitude of event; S. A. Agulhas II; Sea ice observation according to ASPeCt protocol; Sea ice thickness; Sea ice topography; Snow thickness; Snow type; South Atlantic Ocean; Station label; Temperature, air; Temperature, water; Weddell Sea; Wind speed Our knowledge of sea ice variability, which contributes to the detection of the Antarctic climate change trends, stems primarily from remotely sensed information. However, sea ice in the Southern Ocean is characterized by large variability that remains unresolved and limits our confidence on the remotely sensed products. Therefore, the in situ sea ice observations presented (according to the ASPeCt protocol) provide a greater understanding of the Antarctic sea ice environment - on a local scale - and allows us to evaluate remotely sensed products. |
| title | Sea ice conditions within the Antarctic Marginal Ice Zone in summer 2016, onboard the SA Agulhas II |
| topic | AGULII201612; AGULII20161207_10; AGULII20161207_11; AGULII20161207_12; AGULII20161207_13; AGULII20161207_14; AGULII20161207_15; AGULII20161207_16; AGULII20161207_17; AGULII20161207_18; AGULII20161207_19; AGULII20161207_20; AGULII20161207_21; AGULII20161207_22; AGULII20161207_23; AGULII20161207_9; AGULII20161208_0; AGULII20161208_1; AGULII20161208_10; AGULII20161208_11; AGULII20161208_12; AGULII20161208_13; AGULII20161208_14; AGULII20161208_15; AGULII20161208_16; AGULII20161208_17; AGULII20161208_18; AGULII20161208_2; AGULII20161208_3; AGULII20161208_4; AGULII20161208_5; AGULII20161208_6; AGULII20161208_7; AGULII20161208_8; AGULII20161208_9; AGULII20161210_0; AGULII20161210_1; AGULII20161210_10; AGULII20161210_11; AGULII20161210_12; AGULII20161210_13; AGULII20161210_14; AGULII20161210_15; AGULII20161210_16; AGULII20161210_17; AGULII20161210_2; AGULII20161210_3; AGULII20161210_4; AGULII20161210_5; AGULII20161210_6; AGULII20161210_7; AGULII20161210_8; AGULII20161210_9; Comment; Comment of event; DATE/TIME; Event label; Floe size; Ice concentration; ICESUR; Ice survey; Ice type; Latitude of event; Lazarev Sea; Longitude of event; S. A. Agulhas II; Sea ice observation according to ASPeCt protocol; Sea ice thickness; Sea ice topography; Snow thickness; Snow type; South Atlantic Ocean; Station label; Temperature, air; Temperature, water; Weddell Sea; Wind speed |
| url | https://doi.org/10.1594/PANGAEA.885208 |