Information about the Gould Data

General Information

Note on calibration of salinity data

The salinity data are calibrated using a piece-wise linear fit obtained by comparison of float data with WOCE standard CTD casts (see Bacon, Centurioni and Gould, 2001, J. Atm. Oc. Tech., 18,1258).

The correct salinity is obtained with the formula:

Snew = Sold + a + bt,

where t is the time expressed in number of days.

Example (with float 10587):

The following table contains the coefficients a and b and their accuracy, the cycle number that corresponds to the calibration point (that is the float profile for which the comparison with a ship-CTD was made) and the corresponding number of days from the deployment of the float.

Day Cyc. # a delta-a b delta-b
13 1 0.0116 0.0041 -0.000171 0.000656
27 2 0.0092 0.0051 0.000050 0.000156
180 13 0.0168 0.0188 0.000050 0.000294
263 19 0.0210 0.0056 -0.00033 0.001037
276 20 0.0167 0.0079 0.000052 0.000447
303 22 0.0181 0.0042 0 0
0 23 0 0 0 0

To calibrate profile #1: Snew = Sold + 0.0116 + (-0.000171 * 0)

To calibrate profile #2: Snew = Sold + 0.0092 + (-0.000050 * 0)

To calibrate profile #3: Snew = Sold + 0.0092 + (-0.000050 * 14)

To calibrate profile #4: Snew = Sold + 0.0092 + (-0.000050 * 28)

To calibrate profile #13: Snew = Sold + 0.0168 + (-0.000050 * 0)

etc …

Note that since we calculated a piece-wise linear fit, time is counted in days from the most recent calibration event. That is, if t1 = 13, t2 = 27, t3 = 180, t4 = 263 etc are the days corresponding to the calibration events, to calibrate profile #5 the correct formula is:

Snew = Sold + 0.0092 + [-0.000050 * (t2 - t)]

This may appear a bit convoluted and impractical but offsetting the time in this way allows you to appreciate quickly the error in salinity (roughly corresponding to a since the drift, b, is always very small).

Profiles with cycle number > 22 are uncalibrated. The quality of the data is finally checked by plotting a global T/S diagram (with all the calibrated data from the 4 floats). The points with T~< 3 ° C show that the curve is sufficiently tight to assume that the spread of the points in the plot is due to the natural variability of the water mass we are observing (Labrador Sea Water).

Additional salinity calibrations

Float number 10588

Day Cyc. # a delta-a b delta-b
12 1 -0.0276 0.0042 0.000024 0.000042
221 16 -0.0225 0.0045 -0.000089 0.000105
303 22 -0.0298 0.0041 0.000013 0.000161
372 27 -0.0289 0.0070 0 0
0 28 0 0 0 0

Float number 10589

Day Cyc. # a delta-a b delta-b
13 1 -0.0306 0.0044 -0.000053 0.000034
303 22 -0.0461 0.0053 0.000279 0.000198
359 26 -0.0305 0.0058 -0.000862 0.000784
372 27 -0.0417 0.0044 0 0
0 28 0 0 0 0

Float number 10591

Day Cyc. # a delta-a b delta-b
12 1 0.0095 0.0044 0.000736 0.000401
40 3 -0.0111 0.0069 -0.000006 0.000057
234 17 -0.0099 0.0041 -0.000067 0.000208
275 20 -0.0126 0.0044 -0.000226 0.000337
302 22 -0.0187 0.0047 0 0
0 23 0 0 0 0

Pressure offsets

The pressure data have also been adjusted from the original values. The formula is: Pnew = Pold - offset

Absent values for the offset are indicated as -9999

The following tables provide the offsets for each profile for 7 floats.

10587
10588
10589
10590
Offset Profile Number Offset Profile Number Offset Profile Number Offset Profile Number
-6 1 -4 1 -9.1 1 1 1
-10.9 2 -16 2 -15.1 2 -6.9 2
-11.9 3 -15 3 -16.1 3 -3.9 3
-11.9 4 -17 4 -15.1 4 -3 4
-11.9 5 -16 5 -16.1 5 -1 5
-11.9 6 -16 6 -16.1 6 -2 6
-11.9 7 -16 7 -16.1 7 0 7
-11.9 8 -16 8 -16.1 8 -2 8
-11.9 9 -17 9 -16.1 9 0 9
-11.9 10 -17 10 -16.1 10 -2 10
-11.9 11 -16 11 -16.1 11 0 11
-12.9 12 -16 12 -16.1 12 -1 12
-11.9 13 -16 13 -16.1 13 -1 13
-11.9 14 -16 14 -16.1 14 -1 14
-10.9 15 -15 15 -16.1 15 0 15
-10.9 16 -15 16 -15.1 16 0 16
-10.9 17 -16 17 -14.1 17 0 17
-10.9 18 -15 18 -13.1 18 0 18
-9.9 19 -14 19 -13.1 19 0 19
-9.9 20 -14 20 -13.1 20 1 20
-9.9 21 -14 21 -12.1 21 1 21
-9.9 22 -14 22 -12.1 22 1 22
-9.9 23 -14 23 -13.1 23 1 23
-9.9 24 -15 24 -13.1 24 1 24
-9.9 25 -16 25 -14.1 25 1 25
-9.9 26 -16 26 -15.1 26 1 26
-10.9 27 -16 27 -15.1 27 1 27
-12.9 28 -16 28 -15.1 28 0 28
-13.9 29 -17 29 -15.1 29 0 29
-12.9 30 -17 30 -16.1 30 0 30
-11.9 32 -17 31 -16.1 31 0 31
-11.9 33 -17 32 -16.1 32 -1 32
-11.9 34 -17 33

-1 33
-10.9 36 -16 34

-1 34
-10.9 37 -17 35

-1 35
-10.9 38 -17 36

-1 36
-9.9 39 -17 37

-1 37
-8.9 40 -17 38

-1 38
-9.9 41 -17 39

0 39
-8.9 42 -17 40

0 40
-7.9 43 -19 41

0 41
-7.9 44 -18 42

1 42
-6.9 45 -19 43

1 43
-6.9 46 -17 44

1.9 44
-6.9 47 -16 45

1 45
-7.9 48 -15 46

1.9 46
-7.9 49 -14 47

1.9 47
-7.9 50 -15 48

1 48
-7.9 51 -14 49

1 49
-8.9 52 -14 50

1 50
-7.9 53 -14 51

1 51
-8.9 54 -15 52

1 52
-8.9 55 -16 53

0 53
-8.9 56 -17 54

0 54
-8.9 57 -17 55

0 55
-8.9 58 -18 56

0 56
-7.9 59 -18 57

0 57
-7.9 60 -18 58

0 58
-8.9 61 -17 60

0 59
-7.9 62 -18 61

0 60
-6.9 63 -16 62

1 61
-6.9 64 -16 63

0 62
-6.9 65 -16 64

1 63
-6 66 -16 65

0 64
-6 67 -16 66

1 65
-3 68 -15 67

1 66
-3 69 -14 68

1 67
-2 70 -11 69

1 68
-2 71 -9 70

0 69
-1 72 -11 71

1 70
-2 73 -9 72

1 71
-2 74 -9 73

1 72
-3 75 -9 74

1.9 73
-3 76 -5 75

1 74
-5 77 -6 76

1 75
-6 78 -6 77

0 76
-6 79 -7 78

1 77
-6.9 80 -8 79

0 78
-6.9 81 -9 80

0 79
-6.9 82 -8 81

0 80
-7.9 83 -9 82

-1 81
-6.9 84 -9 83

0 82
-7.9 85 -9 84

-2 83
-6.9 86 -9 85

-2 84
-6.9 87 -9 86

-1 85
-7.9 88 -9 87

-2 86
-6.9 89 -10 88

-2 87
-6.9 90 -9 89

-2 88
-4 91 -10 90

-1 89
-6 92 -8 91

-2 90
-6 93 -8 92

-2 91
-2 94 -11 93

-2 92
-1 95 -9 94

-1 93
-1 96 -10 95

-1 94
-1 97 -9 96

-1 95
-1 98 -9999 97

0 96
-1 99 -6 98

-1 97
-1 100 -7 99

-1 98
-1 101 -8 100

-1 99
0 102 -7 101

-1 100
-1 103 -8 102

-3 101
-1 104 -9 103

-3.9 102
-1 105 -9 104

-4.9 103
-1 106 -9 105

-6.9 104
-1 107 -9 106

-7.8 105
0 108 -9 107

-7.8 106
-1 109 -9 108

-8.8 107
-1 110 -9 109

-8.8 108
0 111 -10 110

-9.8 109
0 112 -10 111

-10.8 110
-1 113 -10 112



-10 113



-9 114



-10 115



-9 116



-8 117



-8 118



-7 119



-6 120


10591
10592
10593
Offset Profile Number Offset Profile Number Offset Profile Number
-4.9 1 -5.9 1 -3.1 1
-5.9 2 -9.9 2 -8.3 2
-8.9 3 -12.9 3 -8.3 3


-12.9 4 -7.3 4


-13.9 5 -7.3 5


-12.9 6 -9.3 6


-13.9 7 -9.3 7


-13.9 8 -8.3 8


-13.9 9 -8.3 9


-12.9 10 -8.3 10


-12.9 11 -7.3 11


-11.9 12 -7.3 12


-11.9 13 -7.3 13


-11.9 14 -7.3 14


-10.9 15 -6.2 15


-10.9 16 -6.2 16


-10.9 17 -5.2 17


-8.9 18 -4.1 18


-8.9 19 -3.1 19


-7.9 20 -2 20


-8.9 21 -2 21


-7.9 22 -2 22


-7.9 23 -2 23


-7.9 24 -2 24


-8.9 25 -2 25


-8.9 26 -2 26


-8.9 27 -2 27


-8.9 28 -2 28


-8.9 29 -3.1 29


-8.9 30 -3.1 30




-3.1 31




-4.1 32




-4.1 33




-4.1 34




-4.1 35




-4.1 36




-3.1 37




-3.1 38




-3.1 39




-3.1 40




-2 41




-1 42




0 43




0 44




2.1 45




2.1 46




3.2 47




2.1 48




2.1 49




2.1 50




3.2 51




3.2 52




2.1 53




2.1 54




1.1 55




1.1 56




0 57




1.1 58




0 59




1.1 60




1.1 61




1.1 62




1.1 63




1.1 64




2.1 65




2.1 66




3.2 67




3.2 68




3.2 69




3.2 70




4.2 71




4.2 72




6.3 73




6.3 74




6.3 75




5.3 76




5.3 77




5.3 78




5.3 79




5.3 80




5.3 81




4.2 82




4.2 83




4.2 84




6.3 85




5.3 86




5.3 87




5.3 88




6.3 89




6.3 90




6.3 91




6.3 92




7.3 93




7.3 94




8.4 95




8.4 96




10.5 97




9.4 98




10.5 99




10.5 100




10.5 101




9.4 102




10.5 103




9.4 104




9.4 105




8.4 106




8.4 107




8.4 108




8.4 109




8.4 110




8.4 111




8.4 112




8.4 113




8.4 114




8.4 115




8.4 116




9.4 117




9.4 118




9.4 119




10.5 120




-9999 121




11.5 122




12.6 123




12.6 124




12.6 125




12.6 126




12.6 127