Abstract

The West Antarctic Peninsula (WAP; figure 1) is one of the most climatically sensitive regions on Earth and one of the most variable. The strong climatic variability gives us the opportunity to study and understand how the ocean responds to—and gives feedback on—climate change, and hence to learn about the key mechanisms that are at work, which might apply around the Southern Ocean as a whole. Data coverage is still inadequate across the Southern Ocean (because of remoteness and harsh conditions) and, despite being better observed than many other regions around Antarctica, the nature of oceanographic and atmospheric change on the WAP is poorly constrained. This theme issue addresses some of the most important and pressing questions surrounding marine system variability at the WAP. How has the WAP changed and how will it change in future? What's driving these changes? And why is there such an extraordinary degree of spatial and temporal variability in the region? Figure 1. A map of the Antarctic Peninsula, showing the main islands and ice shelves (grey areas), with research locations mentioned in the text marked with triangles. The main map is an enlarged view of the blue box and was made using etopo1 bathymetry (for bedrock and ice surface files, see https://www.ngdc.noaa.gov/docucomp/page?xml=NOAA/NESDIS/NGDC/MGG/DEM/iso/xml/316.xml&view=getDataView&header=none). These questions were addressed in two interlinked meetings held in 2017. A 2 day meeting was hosted in May at the British Antarctic Survey (BAS) in Cambridge, UK (co-sponsored by the Southern Ocean Observing System, the Scientific Committee for Antarctic Research and the Scientific Committee for Ocean Research), aimed at gathering and critically assessing a broad view from the international community on the gaps and challenges in WAP oceanographic research. A second meeting was held at the Kavli International Centre at Chicheley Hall, UK (funded by the Royal Society), specifically to identify the key …

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