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In fact, the vertical water temperature and salinity profiles we found demonstrate that the mixed layer, determined from both the water temperature and the salinity, becomes deeper almost the entire time that a typhoon passes over.
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NDVI decrease associated with typhoon Herb was only 0.03 (0.93–0.90), at a site in northeastern Taiwan, despite the fact that the typhoon passed directly over northeastern Taiwan.
Around midday (03 00 GMT), the typhoon passed close to Fukushima, where contaminated water used to cool reactor cores is being stored in temporary tanks.
Bands of rain are predicted, some of them heavy, with the centre of the typhoon passing between Monday morning and afternoon.
The salinity in the mixed layer was relatively high on 13 July 2011, before the typhoon passed, but decreased during and after the passage of the typhoon (after July 17), when heavy precipitation occurred.
The analysis period is the period during which the typhoon passed over the area monitored by the profiling floats (Figure 1), and the maximum amount of sea surface cooling, which ranged from 0.8°C to 4.3°C (Table 1), was defined as the difference between the maximum and minimum water temperature at a depth of 5 m during each analysis period.
As they reported that year at a meeting (Science, 23 December 2005, p. 1899), they soon began to notice that slippage on the fault over hours to days that was recorded as changing strain--that is, slow earthquakes--often coincided with a drop in atmospheric pressure as a typhoon passed over.
The following day, the intensifying typhoon passed 165 km southwest of Okinawa.
At 1900 UTC on September 10, the typhoon passed within 10 km (7 mi) of Miyako-jima.
On October 19, a typhoon passed near Wake Island, where a pressure of 968 mbar was recorded.
The typhoon passed offshore of southeastern China and hit western Taiwan on August 22.
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