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 #8 Amundsen - Deceased


Made by MetOcean Data Systems
Iridium ID # (IMEI = International Mobile Equipment Identity): 300234010957610

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 23, 2011 by David Babb (University of Manitoba) in open water from the Canadian Coast Guard Icebreaker Amundsen during their ArcticNet cruise.

Initial status: Unfortunately, all ocean thermistor data from this buoy were unrealiable from the start; we suspect water leakage of some kind. Position and atmospheric and ocean pressure data were good.

THANKS TO: David Barber, chief scientist for this cruise, for allowing us to take time to deploy our buoy, and to David Babb and the ship’s crew for deploying the instrument.




SUMMARY

The plot below shows the path of UpTempO 2011 #8 Amundsen 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 #8 Amundsen
Modem ID (last 4 or 6 digits): 7610

DEPLOYED

Date: 8/23/2011
Position: 74.88N 128.09W
Vessel: Amundsen

LAST TRANSMISSION

Date: 9/ 4/2011
Position: 74.22N 129.54W
Battery Voltage: 14.6V


DOWNLOAD DATA

LEVEL 1 DATA

Data File Size: 92.197 kb

LEVEL 2 DATA

Data File Size: 302.697kb


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.