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Here's a summary of where things stand: Hundreds of thousands of displaced people in the Philippines entered a third night without secure shelter as the central eastern coastline lay destroyed from the passage of typhoon Haiyan on Friday.
The field data, such as wind speed, wind direction and acceleration responses were simultaneously and continuously measured from this building during the passage of Typhoon Sally in 1996.
On the other hand, full-scale measurements of wind actions and wind-induced structural responses of the roof were conducted during the passage of Typhoon Nuri.
In order to prevent the extremely high amount of rainfall brought by typhoon Sinlaku from influencing the results, the survey following the passage of typhoon Sinlaku (September 17th) was not incorporated in the analysis.
The wind speeds and wind direction recorded at different anemometer locations around the Hong Kong area during the passage of Typhoon York are compared with the simulated time histories at these stations.
This paper presents analyzed results of field measurements of wind-induced pressures on building claddings and structural responses of 600 m high Ping-An Finance Center (PAFC) in Shenzhen, China during the passage of Typhoon Haima.
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This paper presents the field measurement results of dynamic characteristics and wind-induced responses of a 420 m high tall building in Hong Kong during the passage of typhoons.
The profiling floats were used to monitor rapid variations in the water temperature and salinity in the upper ocean caused by the passage of typhoons during the 2011 and 2012 seasons.
With meter-thick limestone walls, the type of their infrastructures are designed against the harsh Batanes environment, which is known as a terminal passage of typhoons in the Philippines.
The passage of typhoons, hurricanes, as well as other tropical cyclones have been detected by word of mouth from sailors recently coming to port or by radio transmissions from ships at sea, from sediment deposits in near shore estuaries, to the wiping out of cities near the coastline.
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.
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