UpTempO 2010 #2 Araon - Deceased
Made by MetOcean Data Systems
Iridium ID # (IMEI = International Mobile Equipment Identity): 300034012586420
ocean temperature at nominal depths (m): 2.5, 5.0, 7.5, 10, 15, 20, 25, 30, 35, 40, 50, 60
ocean salinity at nominal depths (m): NA
ocean pressure depths (m): 20, 60
This is a “standard” buoy with the deepest thermistor at 60 m nominal depth. It was deployed on August 9, 2010 by Phil Hwang (Scottish Association for Marine Science) and colleagues from the Korean Polar Research Institute in open water with nearby ice floes during the Arctic Ocean cruise of the Korean icebreaker Araon.
Initial status: All systems working.
PHOTOS
THANKS TO: Phil Hwang (SAMS) and KOPRI colleagues for their work in getting this buoy onto the ship and then onto the ocean.
SUMMARY
The plot below shows the path of UpTempO 2010 #2 Araon colored by month. The flag marks the buoy's last known location. Black contours show two isobaths: 28 m ("short buoy" max depth: e.g., 2011 APLIS buoy) and 60 m ("standard buoy"
max depth).




Buoy Name: UpTempO 2010 #2 Araon
Modem ID (last 4 or 6 digits): 6420
Position: 74.99N 165.00W
Vessel: Araon
Position: 78.16N 169.22E
Battery Voltage: 12.5V
Modem ID (last 4 or 6 digits): 6420
DEPLOYED
Date: 8/ 9/2010Position: 74.99N 165.00W
Vessel: Araon
LAST TRANSMISSION
Date: 12/ 9/2010Position: 78.16N 169.22E
Battery Voltage: 12.5V
DOWNLOAD DATA
LEVEL 1 DATA
Data File Size: 857.896 kbLEVEL 2 DATA
Data File Size: 1068.396kbTEMPERATURE TIME SERIES
The temperature time series for each thermistor is shown below, plotted against day of the year or date.

OCEAN PRESSURE AND SEA LEVEL PRESSURE
This plot shows the ocean pressure(s) from the barometers placed at nominal depths (left axis), and sea level pressure in red (right axis).
BATTERY VOLTAGE/SUBMERGENCE PERCENT
Derived Quantities
VELOCITY TIME SERIES
One to three hourly velocity is on the left axis.Distance between the buoy's start point and end point each day is shown in red on the right axis.Note that the total displacement of the buoy each day (red) is generally less than what one would calculate from the hourly velocities.