The Role of the Atmospheric Circulation in the Record Minimum Extent of Open Water in the
ABSTRACT The contribution of the atmospheric circulation to a record minimum extent of open water in the polar Ross Sea (RS) region in the 2003 austral summer is examined. Two major findings are reached in this study. The first is that the origins of this anomaly are more complex than previously tho...
| Main Authors: | , , , |
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| Other Authors: | |
| Format: | Text |
| Language: | English |
| Published: |
2004
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| Subjects: | |
| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.693.5680 http://www.antarctica.ac.uk/met/wmc/papers/v440106.pdf |
| Summary: | ABSTRACT The contribution of the atmospheric circulation to a record minimum extent of open water in the polar Ross Sea (RS) region in the 2003 austral summer is examined. Two major findings are reached in this study. The first is that the origins of this anomaly are more complex than previously thought, with an anomalous atmospheric circu-lation contributing at least as much to the lack of open water as damming of sea ice by a large iceberg known as C-19. Only in the western RS, where C-19 lay, is damming found to restrict open water in the spring of 2002 (October–December), but even here the coldest spring in the last 15 years extended the sea-ice formation season. Elsewhere in the RS the divergent northward ice drift that normally occurs widely reversed to southward in early spring and was then followed by negligible ice motion. The most anomalous springtime ice drift occurred in the cen-tral and eastern RS rather than near C-19 and was mirrored in the weakest southerly winds on record in central areas. The unusual southward ice drift in early spring 2002 caused widespread convergence and compaction of the normally thin and undeformed first-year ice along and north of the central and eastern Ross Ice Shelf (RIS). Compacted ice with few leads would have been slow to melt in the warmest summer (January–February) months. Direct observations also indicate that sea surface temperatures (SSTs) rapidly fell to freezing in the central and western RS in February 2003 supporting new ice formation. All the available data indicate these were due to the cold spring and the extensive, compact ice cover in the late spring of 2002 and in January 2003 preventing most |
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