Table 2
(continued)
Section
FBTE
⟨δQ⟩
(Sv),
see (21)
Deviation
∑ Δζ
t (cm),
see (6b)
Deviation
Q
t (Sv),
see (10)
b
Range
ΔQ adcp t
ð Þ (Sv),
see (11)
c
Range
ΔQ
0
alt t
ð Þ (Sv),
see (15)
c
Discrepancy
ΔQ (Sv),
see (17);
SLA(ADT)
Range
ΔQ − ΔQ t
ð Þ
(Sv),
see (18)
Range
Q
adcp
− Q ̄
adcp
(Sv),
see (25)
A10 2011
10.0
2.86
16.6
−14.9 to 43.2
−30.2 to 29.2
−2.0(−2.6)
−3.3 to 0.8
−0.3
I05 2002
11.7
1.42
5.7
−67.0 to 85.2
−60.2 to 89.4 0.1(−1.9)
−15.3 to 18.1
−9.5
I05 2009
10.9
3.55
15.6
−184.2 to
166.7
−201.3 to
150.4
−0.5(0.4)
12.8 to 20.5
−3.4
P02 1994
33.7
−4.79
−32.6
−45.1 to 57.7
−44.1 to 89.1 8.6(−21.4)
−33.0 to 31.8
−28.1
P02 2004
14.5
15.82
88.0
−331.1 to
153.2
−416.4 to
64.0
−0.5(−1.9)
−3.6 to 14.8
−5.3
P02 2013
16.9
−7.37
−43.2
−249.5 to
−57.9
−191.2 to
−0.1
−13.8(−14.5)
−23.8 to
−3.3
−2.0
P06 2003
8.2
3.69
13.6
11.4 to 293.7
−7.8 to 276.4 1.8(2.4)
−1.6 to 11.1
−5.7
P06 2009
9.4
−5.32
−37.1
−128.4 to
234.4
−85.4 to
282.0
−3.2(−2.9)
−12.6 to 4.1
−4.6
a
The estimates for the SR02 sections in 1995 and 1996 are given for the entire section, except for a small southern segment, enclosed in the data by an ice mask
b
Bold face in this column indicates the transport deviations greater than FBTE
c
Bold face in this column corresponds to the ranges of the transport variability that do not cross the zero line
Influence of the Current Field Non-stationarity …
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