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The sensors on JKEO1 are as same as on the KEO.
The following description is based on that in KEO web site. The
table below identifies the types of sensors used on JKEO1 moorings and lists
their specifications. Most instrumental accuracies listed are based on
historical pre-deployment and post-recovery calibrations and are the root
mean square drift of a group of sensors. References where available are
indicated by [#] in the comments column and listed at the end of the tables.
Accuracies of sensors which have not been evaluated by the JKEO1, KEO or TAO project offices (i.e.
longwave radiation, wind speed and direction, water pressure) are those
specified by the manufacturer and are indicated by [M]. In
cases where sensors are paired with PMEL
supplied electronics (e.g., analog to digital boards) calibrations include
both the sensor and PMEL electronics. Accuracies listed here (with the
exception of currents) do not include environmental factors such as wind (on
rainfall) or buoy motion (on radiation). Measurement ranges listed are
generally those over which the sensors are calibrated. The ranges over which
a sensor will operate (determined by the sensor and/or PMEL electronics) are
listed in parenthesis if they significantly exceed the calibration range. Last updated on December 26, 2008
Note: ATLAS = Automated Temperature
Line Aquisition Systerm [1]
Fairall, C. W., P. O. G. Persson, E.F. Bradley, R. E. Payne and S. P.
Anderson, 1998: A new look at calibration and use of Eppley Precision
Radiometers. Part I: Theory and Application. J.
[2]
Freitag, H.P., Y. Feng, L.J. Mangum, M.J. McPhaden, J. Neander, and L.D.
Stratton, 1994: Calibration procedures and instrumental accuracy estimates of
TAO temperature, relative humidity and radiation measurements. NOAA Tech. Memo. ERL PMEL-104,
32 pp. [3] Freitag,
H.P., M.E. McCarty, C. Nosse, R. Lukas, M.J. McPhaden, and M.F. Cronin, 1999:
COARE Seacat data: Calibrations and quality control procedures. NOAA Tech. Memo. ERL PMEL-115,
89 pp. [4]
Halpern, D., 1987: Comparison of upper ocean VACM and VMCM observations in
the equatorial Pacific. J. [5]
Plimpton, P.E., H.P. Freitag, and M.J. McPhaden, 1995: Correcting moored ADCP
data for fish-bias errors at 0°,110°W and 0°,140°W from 1990 to 1993. NOAA Tech. Memo. ERL PMEL-107,
49 pp. [6] Serra,
Y.L., P.A'Hearn, H.P. Freitag, and M.J. McPhaden, 2001: ATLAS self-siphoning rain
gauge error estimates. J. [7]
Freitag, H.P., M. O'Haleck, G.C. Thomas, and M.J. McPhaden, 2001: Calibration
procedures and instrumental accuracies for ATLAS wind measurements. NOAA.
Tech. Memo. OAR PMEL-119, NOAA/Pacific Marine Environmental Laboratory, [8]
[9]
A'Hearn, P.N., H.P. Freitag, and M.J. McPhaden, 2002: ATLAS module
temperature bias due to solar heating. NOAA Tech. Memo OAR PMEL-121, NOAA/Pacific
Marine Environmental Laboratory, [10] Freitag,
H.P., M.J. McPhaden, C.Meinig, and P.Plimpton, 2003: Mooring motion bias of
point Doppler current meter measurements. In: Proceedings of the IEEE Seventh
Working Conference on Current Measurement Technology, San Diego, CA, 13-15
March 2003, IEEE, Piscataway, NJ, 155-160. [11] Plimpton,
P.E., H.P. Freitag, and M.J. McPhaden, 2004: Processing of subsurface ADCP
data in the equatorial Pacific. NOAA Tech. Memo OAR PMEL-125, NOAA/Pacific
Marine Environmental Laboratory, [12]
[13]
Payne, R.E., K. Huang, R.A. Weller, H.P. Freitag, M.F. Cronin, M.J. McPhaden,
C. Meinig, Y. Kuroda, N. Ushijima, R.M. Reynolds, 2002: A comparison of buoy
meteorological systems. WHOI Technical Report |
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Home/Overview
| Technical Info | Data![]()
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Kuroshio Transport and Surface
Flux Group, Ocean General Circulation
Observational Research Program, Institute of Observational
Research for Global Change (IORGC), Japan Agency for Marine-Earth
Science and Technology (JAMSTEC) 2-15 Natsushima-cho
Yokosuka-city,Kanagawa, 237-0061, |
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JKEO web master |