UpTempO


Measuring the Upper layer Temperature of the Polar Oceans

UpTempO 2024: NOAA Twin Otter #1| NOAA Twin Otter #2| NOAA Twin Otter #3| NOAA Twin Otter #4| NOAA Twin Otter #5| NOAA Twin Otter #6| SIZRS #7| NOAA Twin Otter #8| NOAA Twin Otter #9| NOAA Twin Otter #10| NOAA Twin Otter #11| NOAA Twin Otter #12|
UpTempO 2023: NOAA Twin Otter #1| NOAA Twin Otter #2| NOAA Twin Otter #3| NOAA Twin Otter #4| HEALY #5| HEALY #6| HEALY #7| MIRAI #8| NOAA Twin Otter #9| NOAA Twin Otter #10| NOAA Twin Otter #11| NOAA Twin Otter #12| SIZRS #13|
UpTempO 2022: SASSIE #1| SASSIE #2| SASSIE #3| SASSIE #4| SASSIE #5| SASSIE #6| SASSIE #7| SASSIE #8| SASSIE #9| SASSIE #10| SASSIE #11| SIZRS #12|
UpTempO 2021: SIZRS #1| SIZRS #2| SIZRS #3| SIZRS #4| SIZRS #5|
UpTempO 2020: JWARM #2| MIRAI #1|
UpTempO 2019: WARM #9| SIZRS #1| SIZRS #2| SIZRS #3| MOSAiC #4| MOSAiC #5|
UpTempO 2018: JWARM #1| WARM #7| WARM #8| AMUNDSEN #1| SIZRS #2|
UpTempO 2017: WARM #5| WARM #6| SIZRS #1| SIKULIAQ #2| MIRAI #3| HEALY #4| Laurier #5|
UpTempO 2016: ICEX #1| HEALY #2| ARAON #3| UKPIK #4| AMUNDSEN #5| AMUNDSEN #6| HEALY #7| AMUNDSEN #8| SIKULIAQ #9|
UpTempO 2015: HEALY #1| SIZRS #2| SIZRS #3| SIZRS #4| SIZRS #5| HEALY #6| HEALY #7| SIZRS #8|| WARM #3| WARM #4
UpTempO 2014: APLIS #1| APLIS #2| SIZRS #3| SIZRS #4| AARON #5| SIZRS #6| SIZRS #7| AARON #8| AMUNDSEN #9| AMUNDSEN #10| AMUNDSEN #11| POLARSTERN #12| MIRAI #13| MIRAI #14| MIRAI #15| POLARSTERN #16|| WARM #1| WARM #2
UpTempO 2013: PALMER #1| PALMER #2| PALMER #3| UKPIK #4| LOUIS #5| SIZRS #6| LOUIS #7| LOUIS #8| LOUIS #9| LOUIS #10| ARAON #11| ARAON #12| HEALY #13| ARAON #14| FEDEROV #15| HEALY #16| HEALY #17| HEALY #18| FEDEROV #19| FEDEROV #20|
UpTempO 2012: PALMER #1| LOUIS #2| LOUIS #3| LOUIS #4| LOUIS #5| POLAR STERN #6| HEALY #7| POLAR STERN #8|
UpTempO 2011: APLIS #1| HEALY #2| LOUIS #3| LOUIS #4| ARAON #5| ARAON #6| HEALY #7| AMUNDSEN #8| AMUNDSEN #9| LAURIER #10
UpTempO 2010: ARAON #1| ARAON #2| AMUNDSEN #3










UpTempO 2011 #5 Araon - Deceased


Made by MetOcean Data Systems
Iridium ID # (IMEI = International Mobile Equipment Identity): 300234010956630

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 8, 2011 by Phil Hwang (Scottish Association for Marine Science) and colleagues from the Korean Polar Research Institute in an ice floe during the Arctic Ocean cruise of the Korean icebreaker Araon.

Initial status: Within 2 days, most ocean thermistors began to give unrealistic values. Position and atmospheric/oceanic pressure data were unaffected.

PHOTOS

THANKS TO: Phil Hwang (SAMS) and KOPRI colleagues for their work in getting this buoy onto the ship and then onto the ice.




SUMMARY

The plot below shows the path of UpTempO 2011 #5 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 2011 #5 Araon
Modem ID (last 4 or 6 digits): 6630

DEPLOYED

Date: 8/ 8/2011
Position: 77.77N 162.29W
Vessel: Araon

LAST TRANSMISSION

Date: 5/22/2013
Position: 71.96N 155.90W
Battery Voltage: 11.7V


DOWNLOAD DATA

LEVEL 1 DATA

Data File Size: 4153.083 kb

LEVEL 2 DATA

Data File Size: 4363.583kb


TEMPERATURE 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.