Haardt, H; Maaßen, R (1983): Oceanographic and optical profile at station M56_26-29 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.80657, In supplement to: Haardt, H; Maaßen, R (1983): CTD and optical data from the Antarctic - Meteor 56 ANT I - Part I: CTD and Chlorophyll profiles. Reports Sonderforschungsbereich 95 Wechselwirkung Meer-Meeresboden, 61, 8 pp, tables digital, hdl:10013/epic.35197.d001
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Coverage:
Latitude: -62.958100 * Longitude: -54.726700
Date/Time Start: 1980-11-25T06:35:00 * Date/Time End: 1980-11-25T06:35:00
Minimum DEPTH, water: 1 m * Maximum DEPTH, water: 267 m
Event(s):
M56_26-29 * Latitude: -62.958100 * Longitude: -54.726700 * Date/Time: 1980-11-25T06:35:00 * Elevation: -271.0 m * Campaign: M56 (FIBEX - First International BIOMASS Experiment, ANT I) * Basis: Meteor (1964) * Method/Device: Multisonde (MS)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, water | Depth water | m | Geocode | ||
2 | Pressure, water | Press | dbar | Haardt, H | CTD | |
3 | Temperature, water | Temp | °C | Haardt, H | see comment | The variation of the electrical resistance of a platinum thermometer is converted to an analogous frequency variation by using a relaxation oscillator. The thermometers are calibrated against a set of standard thermometers with an accuracy of 0.02 deg C |
4 | Attenuation, optical beam transmission | Attenuation | 1/m | Haardt, H | CTD | |
5 | Chlorophyll fluorescence raw data | Chl fluores | V | Haardt, H | Chlorophyll fluorescence, Dr. Haardt Instruments | |
6 | Irradiance, heat, flux density | E | W/m2 | Haardt, H | CTD |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
229 data points
Data
1 Depth water [m] | 2 Press [dbar] | 3 Temp [°C] | 4 Attenuation [1/m] | 5 Chl fluores [V] | 6 E [W/m2] |
---|---|---|---|---|---|
1 | 0.6 | -1.750 | 0.86 | 2.30 | -1.15 |
2 | 1.5 | -1.725 | 0.76 | 1.69 | -1.28 |
2 | 1.5 | -1.734 | 0.69 | 1.20 | -1.30 |
2 | 1.5 | -1.737 | 0.68 | 1.94 | -1.28 |
2 | 1.5 | -1.744 | 0.76 | 1.41 | -1.29 |
5 | 4.6 | -1.750 | 0.72 | 1.23 | -1.64 |
10 | 10.3 | -1.750 | 0.70 | 2.09 | -2.06 |
16 | 16.1 | -1.750 | 0.68 | 1.54 | -3.39 |
22 | 21.7 | -1.744 | 0.69 | 1.25 | -2.70 |
27 | 27.3 | -1.741 | 0.74 | 1.34 | -2.99 |
33 | 33.0 | -1.741 | 0.70 | 1.16 | -3.29 |
39 | 38.8 | -1.737 | 0.68 | 1.93 | -3.57 |
44 | 44.4 | -1.734 | 0.70 | 0.96 | -3.86 |
50 | 50.3 | -1.734 | 0.72 | 1.24 | -4.13 |
56 | 56.0 | -1.737 | 0.76 | 1.12 | -4.41 |
61 | 61.7 | -1.737 | 0.72 | 1.38 | -4.69 |
67 | 67.3 | -1.737 | 0.70 | 1.44 | -4.96 |
72 | 73.1 | -1.737 | 0.69 | 1.29 | |
78 | 78.7 | -1.737 | 0.71 | 1.53 | |
84 | 84.4 | -1.737 | 0.68 | 1.12 | |
89 | 90.0 | -1.737 | 0.69 | 1.56 | |
95 | 96.1 | -1.737 | 0.69 | 0.86 | |
101 | 101.9 | -1.737 | 0.71 | 1.45 | |
107 | 107.6 | -1.741 | 0.72 | 1.40 | |
112 | 113.3 | -1.744 | 0.70 | 0.55 | |
118 | 119.0 | -1.744 | 0.69 | 1.12 | |
123 | 124.5 | -1.747 | 0.73 | 1.66 | |
129 | 130.1 | -1.744 | 0.69 | 1.87 | |
135 | 135.8 | -1.750 | 0.76 | 0.95 | |
140 | 141.3 | -1.750 | 0.70 | 2.03 | |
146 | 147.0 | -1.750 | 0.74 | 0.90 | |
151 | 152.5 | -1.747 | 0.74 | 1.81 | |
156 | 157.8 | -1.750 | 0.70 | 1.63 | |
162 | 163.6 | -1.750 | 0.67 | 1.18 | |
167 | 169.1 | -1.750 | 0.74 | 1.02 | |
173 | 174.7 | -1.750 | 0.72 | 0.87 | |
179 | 180.5 | -1.750 | 0.69 | 1.25 | |
184 | 186.2 | -1.756 | 0.70 | 1.09 | |
190 | 192.0 | -1.756 | 0.69 | 1.21 | |
196 | 197.6 | -1.756 | 0.68 | 0.89 | |
202 | 203.5 | -1.756 | 0.70 | 1.03 | |
207 | 209.2 | -1.756 | 0.74 | 1.50 | |
213 | 215.0 | -1.756 | 0.74 | 1.44 | |
219 | 220.9 | -1.762 | 0.70 | 2.16 | |
224 | 226.2 | -1.759 | 0.70 | 1.13 | |
230 | 231.8 | -1.771 | 0.76 | 0.85 | |
235 | 237.3 | -1.771 | 0.72 | 1.22 | |
240 | 242.8 | -1.774 | 0.74 | 1.20 | |
246 | 248.3 | -1.771 | 0.73 | 1.31 | |
251 | 253.7 | -1.774 | 0.73 | 0.85 | |
257 | 259.1 | -1.771 | 0.77 | 0.96 | |
262 | 264.5 | -1.774 | 0.74 | 0.80 | |
267 | 269.3 | -1.774 | 0.83 | 0.84 |