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- W1978562309 abstract "A preliminary examination of the winds and sea surface temperatures in the 120‐year record of ocean climate produced by the Historical Sea Surface Temperature Project has provided evidence of two distinct ocean‐wide modes of variability. One of these has a typical time scale of a few years and is closely related to the EI Niño phenomenon. The other has a time scale of the order of 30–100 years and has exhibited sharp changes in higher southern latitudes. However, the uneven distribution of the marine observations in space and time is a potential source of spurious anomaly changes. A comparison of average ship winds for different‐sized areas with winds derived for the same areas from weather charts is presented to illustrate the limited significance that can be attached to the local anomalies; this points up a need for the joint interpretation of anomaly changes over wider areas as resulting from changes in the characteristic behavior of synoptic pressure systems. A tentative explanation of the nearly simultaneous changes in the winds and sea surface temperatures of the latitude belt 40°S to 50°S is derived from Wyrtki's (1960, 1961) circulation model for the Southern Ocean. That region apparently plays a leading role in the long‐term fluctuations of ocean climate through the Antarctic Intermediate Water and Sub‐Antarctic Mode Water. These water masses acquire their characteristics from the surface energy balance and sea ice processes in high southern latitudes and occupy a deep layer extending up to just below the thermocline in the tropical ocean; it is suggested that they could be a pathway for climatic signals from the Antarctic Ocean to the rest of the globe." @default.
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- W1978562309 date "1982-05-20" @default.
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- W1978562309 title "Climatic signals of the Antarctic Ocean" @default.
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- W1978562309 doi "https://doi.org/10.1029/jc087ic06p04269" @default.
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