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Observations of water temperature and salinity in Ongul Strait, Antarctica, in 1998 and investigations of their intraseasonal, seasonal, and interannual variations

机译:1998年在南极洲翁古尔海峡观测水温和盐度,并研究其季节内,季节和年际变化

摘要

Water temperature and salinity variations were observed below fast ice in Ongul Strait, Antarctica, in 1998. Vertical profiles of temperature and salinity were obtained with a conductivity-temperature-depth profiler, and temperature and salinity were continuously observed with moored sensors. Intraseasonal variations were observed in both fields. Especially, temperature variation of about 0.05℃ was apparent on the time scale of about one month near the thermocline depth. Seasonal variations of temperature and salinity were similar to those observed in 1982-1983 and 1990-1991. However, the temporally averaged temperature and salinity for 1998 showed differences from those for previous years; temperature was higher in 1998 than in 1982-1983 and 1990-1991 at middle to deep layers, and salinity was intermediate between 1982 (more saline) and 1990-1991 (fresher) throughout the water column.
机译:1998年,在南极省Ongul海峡的速冻冰下观察到水温和盐度变化。使用电导率-温度-深度剖面仪获得温度和盐度的垂直剖面,并使用系泊传感器连续观察温度和盐度。在两个领域均观察到季节内变化。特别是,在接近温跃层深度的约一个月的时间尺度上,温度变化约为0.05℃。温度和盐度的季节性变化与1982-1983年和1990-1991年的变化相似。然而,1998年的时间平均温度和盐度与往年相比有所不同;在中层至深层,1998年的温度高于1982-1983年和1990-1991年,并且在整个水柱中,盐度介于1982年(含盐量更高)和1990-1991年(淡水剂)之间。

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