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国家海洋技术中心根据科研需求研发了抛弃式温度剖面仪(XBT)等一系列抛弃式产品.针对2014年8月份在西太平洋海域投放的XBT和XCTD所获取的温度数据进行对比分析,单剖面结果显示两者相关系数达到了0.95,在温跃层处出现温度差,断面标准差分析结果为200 m以上温跃层处较大而200m以下标准差较小,最大和最小标准差值分别为0.39和0.08.温度断面分析结果显示两者在同样的位置出现等值线的凹凸现象,对大洋水团特殊物理海洋现象描述基本一致.分析温跃层处两者温度存在偏差的原因有3个:不同传感器的不同响应时间引起的误差、深度测量公式的误差以及传感器本身的测量误差影响.国产XBT的数据质量较好,总体上性能能满足对环境复杂海域的快速走航观测,数据质量准确度和可靠性都较好. 相似文献
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Observations of the Kuroshio south of Taiwan have been carried out on a quarterly basis since late 1992 as part of the basin-wide
High Resolution expendable bathythermograph/expendable conductivity-temperature-depth (XBT/XCTD) network. Mean geostrophic
transport in the Kuroshio, 0–800 m, from 34 cruises is 22.0 Sv ± 1.5, consistent with previous results from moorings and geostrophic
calculations in the upstream Kuroshio region. The mean core of the current has speed about 90 cm s−1 and is located close to Taiwan. At this location the Kuroshio appears to be confined mainly to the upper 700 m, and there
is no evident tight recirculation of the current. Eddy variability is substantial, and large eddies can be seen propagating
westward for thousands of kilometers in TOPEX/Poseidon altimetric data, impinging on the current and altering its structure
and transport. The annual range in transport is about 8 Sv ± 6, with maximum in summer. Interannual variability is about 12
Sv ± 6, with transport maxima in 1995 and 2000 and a minimum in 1997–1998. Interannual variability in the upstream Kuroshio
may be uncorrelated with that in the downstream region south of Japan, where the transport is much greater. Our quarterly
sampling aliases high frequency variability of the current, and an improved boundary-current observation program would include
more frequent transects and occasional deeper measurements.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
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XCTD定标方法研究 总被引：2，自引：0，他引：2
文章简要介绍了投弃式电导率、温度、深度剖面测量仪(XCTD)的定标原理,并对现行的两种定标方法—五点定标和三点定标方法进行了比较研究。指出:与五点定标相比,三点定标方法具有高效、快速的优点,更适于大批量生产的要求。 相似文献
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Preliminary results of in-situ XCTD/CTD comparison test 总被引：4，自引：0，他引：4
The current status of XCTD manufactured by the Tsurumi Seiki Co. is described based on XCTD/CTD comparison tests conducted
in the Pacific and Indian Ocean in November 1996 and January 1997 respectively. The falling rates of used probes are generally
consistent and differences between individual probes stay within a small range of +/−5 m through the full depth range (0–1000
m), although the rate is slightly different from the depth-time equation provided by the manufacturer. Temperature and salinity
accuracy is estimated to be better than 0.05°C and 0.05 psu respectively. Comparison of vertical temperature/salinity sections
of XCTD/CTD constructed separately along a line on which XCTD stations locate midway of CTD stations. The hydrographic structures
obtained are generally consistent, and the difference of surface dynamic height (referred to 1000 db) is 0.03 dyn m in RMS. 相似文献
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Takashi Yabuki Toshio Suga Kimio Hanawa Koji Matsuoka Hiroshi Kiwada Tomowo Watanabe 《Journal of Oceanography》2006,62(5):649-655
It has been inferred that the Prydz Bay region is one of the source regions of Antarctic Bottom Water (AABW) based on rather
indirect evidence. In order to examine this inference, we investigate the hydrographic condition of the bay based mainly on
XCTD data obtained during the Japanese Whale Research Program in the Antarctic (JARPA). The JARPA hydrographic data reveal
Circumpolar Deep Water (CDW), which is a salty, warm water mass approaching the shelf break, and capture Modified CDW (MCDW)
intruding into the shelf water. AABW production requires mixing of CDW and cold shelf water saltier than 34.6 psu, which is
a saltier type of Low Salinity Shelf Water (LSSW). Saltier LSSW is observed near the bottom over the shelf, being mixed with
MCDW. We further identify saltier LSSW near the shelf break. This saltier LSSW appears close enough to unmodified CDW to be
mixed with it over the continental slope, indicating a possible source of AABW in Prydz Bay. 相似文献
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