4.7 Article

Interannual Climate Variability in the West Antarctic Peninsula under Austral Summer Conditions

期刊

REMOTE SENSING
卷 13, 期 6, 页码 -

出版社

MDPI
DOI: 10.3390/rs13061122

关键词

climate variability; West Antarctic Peninsula (WAP); SST; multi-sensor LAC imagery; five-year warm cycle; Southern Annular Mode (SAM); Antarctic Oscillation (AAO); Southern Oscillation Index (SOI); WAP marine ecoregions; Group on Earth Observations (GEO)

资金

  1. Universidad Autonoma de Baja California
  2. AmeriGEOSS
  3. CONACYT [CB-2012-01/179753]

向作者/读者索取更多资源

This study aimed to describe interannual climate variability in the West Antarctic Peninsula, finding a pattern of warm followed by cold episodes and the presence of warm waters near the coast during warm episodes. The WAP can be divided into two ecoregions, and the Southern Annular Mode was identified as the primary driver of SST variability. Further research is needed to better understand regional climate variability in the WAP and its relation with SAM and ENSO.
This study aimed to describe the interannual climate variability in the West Antarctic Peninsula (WAP) under austral summer conditions. Time series of January sea-surface temperature (SST) at 1 km spatial resolution from satellite-based multi-sensor data from Moderate Resolution Imaging Spectrometer (MODIS) Terra, MODIS Aqua, and Visible Infrared Imager Radiometer Suite (VIIRS) were compiled between 2001 and 2020 at localities near the Gerlache Strait and the Carlini, Palmer, and Rothera research stations. The results revealed a well-marked spatial-temporal variability in SST at the WAP, with a one-year warm episode followed by a five-year cold episode. Warm waters (SST > 0 degrees C) reach the coast during warm episodes but remain far from the shore during cold episodes. This behavior of warm waters may be related to the regional variability of the Antarctic Circumpolar Current, particularly when the South Polar Front (carrying warm waters) reaches the WAP coast. The WAP can be divided into two zones representing two distinct ecoregions: the northern zone (including the Carlini and Gerlache stations) corresponds to the South Shetland Islands ecoregion, and the southern zone (including the Palmer and Rothera stations) corresponds to the Antarctic Peninsula ecoregion. The Gerlache Strait is likely situated on the border between the two ecoregions but under a greater influence of the northern zone. Our data showed that the Southern Annular Mode (SAM) is the primary driver of SST variability, while the El Nino Southern Oscillation (ENSO) plays a secondary role. However, further studies are needed to better understand regional climate variability in the WAP and its relation with SAM and ENSO; such studies should use an index that adequately describes the ENSO in these latitudes and addresses the limitations of the databases used for this purpose. Multi-sensor data are useful in describing the complex climate variability resulting from the combination of local and regional processes that elicit different responses across the WAP. It is also essential to continue improving SST approximations at high latitudes.

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