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García-Herrera, Ricardo; Können, Gunther P; Wheeler, Dennis A; Prieto, Maria del Rosario; Jones, Philip D; Koek, Frits B (2010): Meteorological observations during Götha Leijon cruise from Macao to Gothenburg started at 1752-01-06 [dataset]. Gothenburg University Library, Gothenburg, Sweden, PANGAEA, https://doi.org/10.1594/PANGAEA.746929, In: Jones, Philip D; Wheeler, Dennis A; Können, Gunther P; Koek, Frits B; Prieto, Maria del Rosario; García-Herrera, Ricardo (2007): Climatological observations from ship logbooks between 1750 and 1854 (release 2.1) [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.611088

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Related to:
García-Herrera, Ricardo; Können, Gunther P; Wheeler, Dennis A; Prieto, Maria del Rosario; Jones, Philip D; Koek, Frits B (2005): CLIWOC: A Climatological Database for the World's Oceans 1750–1854 (and 10 more publications about CLIWOC results in the same volume). Climatic Change, 73(1-2), 1-12ff, https://doi.org/10.1007/s10584-005-6952-6
Funding:
Fifth Framework Programme (FP5), grant/award no. EVK2-CT-2000-00090: Climatological Database for the Worlds Oceans: 1750-1854
Coverage:
Median Latitude: 1.079686 * Median Longitude: 13.942264 * South-bound Latitude: -35.770000 * West-bound Longitude: -38.210000 * North-bound Latitude: 57.280000 * East-bound Longitude: 115.150000
Event(s):
Götha_Leijon_17520106_GUBSOKAH-22-3_1291 * Latitude Start: 21.700000 * Longitude Start: 113.857000 * Latitude End: 57.670000 * Longitude End: 11.250000 * Campaign: Cliwoc_cruise * Method/Device: Underway cruise track measurements (CT) * Comment: Ship: Götha Leijon, Start of voyage: 1752-01-06, End of voyage: 1752-06-26, Voyage: Macao - Gothenburg, 1st Observer: C.H. Braad (Clerk), Company: Swedish East India Company
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Date/time startDate/time start
2LATITUDELatitudeGeocode
3LONGITUDELongitudeGeocode
4Temperature, airTTT°C
5LandmarkLandmarkName of first landmark
6--1 If position is considered to be coastal (in port or near coastal disturbances)
7DeclinationDecldegIt is generally accepted by the CLIWOC team that the wind directions, reported by the ships officers, were relative to the magnetic North direction. Navigators were well aware of the difference between the true and magnetic north direction, but the compasses (we assumed that the bearing-compasses were mostly used for determining the wind direction) were not always adjusted. Therefore the wind direction has to be corrected. The magnetic declination (or variation, as it is known on board ships) is given for the whole CLIWOC period (1750-1850) for every 5x5 degree square. The number was added to the wind direction to get the true wind direction.
8Sensor readingReadingarbitrary unitsReading of the (outside) air thermometer
9GustsGusts1 If wind gusts are reported
10Precipitation/RainRain1 If rain was reported
11FogFog1 If fog was reported
12Snow typeSnow1 If snow was reported
13ThunderThunder1 If thunder and or lightning was reported
14HailHail1 If hail was reported
15Sea iceSea ice1 If sea-ice or icebergs were reported
16CommentComment
17IdentificationIDCLIWOC 2.1 line number
Size:
2078 data points

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