MATHEMATICAL NOTATIONS
507
J
salinity flux
(1.11)
1.2.2
J rV
volume source of freshwater due to the decay of
raindrops
(1.11)
1.2.2
k
wavenumber (
2 /
k S O )
(1.102) 1.6.2
k
G
wavenumber vector with components ,
x
y
k k
(1.100) 1.6.2
K b
bubble-mediated transfer velocity
(7.26)
7.5.3
K B
turbulent diffusion coefficient for bubbles
(6.10)
6.1.4
K D
turbulent diffusion coefficient for droplets
(6.17)
6.2.2
K h
horizontal mixing coefficient
(5.16)
5.3.7
K int
interfacial (direct) transfer velocity
(7.23)
7.5.2
K Ci
diffusion coefficient for i-th tracer
(1.15)
1.2.2
Ke
Keulegan number
(2.1)
2.2.3
K M
kinematic viscosity
(1.5)
1.2.1
K S
diffusion coefficient for salinity
(1.14)
1.2.2
K T
thermal diffusion coefficient
(1.13)
1.2.2
K P
gas transfer (piston) velocity
(1.44)
1.3.2
K 0
mixing coefficient in the logarithmic boundary
layer
(3.93)
3.4.2
l
characteristic length scale of turbulence
(3.30)
3.3.2
L
width of frontal interface
5.4.4
L
specific heat of vaporization for water
(1.28)
1.3.1
, ,
L z T I
radiance in the direction defined by the zenith
angle T and azimuth angle I , and z is the
depth
(1.47)
1.4.1
L c
diameter of low-salinity lense
5.3.5
L E
Ekman length scale
(3.5)
3.1.2
L f
baroclinic Rossby radius
5.3.5
L G
Garwood et al. (1985) length scale
3.5.3
L O
Oboukhov buoyancy length scale
(3.6)
3.1.2
L p
pressure-gradient length scales
3.5.4
L E
equatorial baroclinic Rossby radius
5.3.1
m d
mass of the free-ascending device
(3.9)
3.2.4
M r
cumulative precipitation
(4.27)
4.2.4
n(r 0 )
initial drop size distribution (at z = 0)
(1.65)
1.5.2
N
Brunt-Vaisala frequency
(3.98)
3.4.3
Nu
Nusselt number
(2.66)
2.3.3
p
pressure
(1.1)
1.2.1
p a
gas partial pressure in air
(1.45)
1.3.2
p w
gas partial pressure in water
(1.45)
1.3.2
p 0
atmospheric pressure
(1.93)
1.6.1