rootone said:
Easterly blowing trade winds at the surface are probably the most famous example of established wind patterns which move large volumes of air from east to west.
https://en.wikipedia.org/wiki/Trade_winds
Thank you for that citation on the trade wind. In reading it, I could find no substantiation of your notion that "The net effect for the atmosphere as a whole is zero movement in relation to the surface," and that the tradewinds move a larger volume of air than the jet streams. On the other hand, I have found numerous references which tend to suggest a net movement west to east. Atmospheric Angular Momentum (AAM) and Length of Day (LOD)
http://onlinelibrary.wiley.com/doi/10.1029/2006RG000213/full
[2] Angular momentum characterizes the rotation of physical systems ranging from the atomic scale to galaxies. In particular, the global angular momentum M of the atmosphere reflects both the rotation tied to that of the Earth and rotation due to the winds. A wealth of data and theories is available to determine the distribution of angular momentum and to provide the reasons for its changes. Attention is restricted in this review to large-scale motions, although angular momentum is also of key importance, say, in hurricanes or tornadoes. The global atmospheric angular momentum is the integral
http://onlinelibrary.wiley.com/store/10.1029/2006RG000213/asset/equation/rog1654-math-0001.gif?v=1&t=ippj8s7t&s=2c2bab9f874ffdbedcaaf572f9d2096c39ec53ce
of the angular momentum
http://onlinelibrary.wiley.com/store/10.1029/2006RG000213/asset/equation/rog1654-math-0002.gif?v=1&t=ippj8s7t&s=518c5825d4839641914d971653bfaf4b0138cb78
per unit volume over the volume
V of the Earth's atmosphere. In
(2), r is the position vector pointing from the center of the Earth to the volume element
dV of density
ρ (see
Figure 1). It is customary to assume a dry atmosphere because the contribution of the water substance to the total mass of the atmosphere is small. In principle, the density
ρ in
(2) also contains the water substance in all phases. The rotation of the Earth is represented by its angular velocity Ω with Ω = 2
π/
d. The relative velocity of the air with respect to this rotation is v and
http://onlinelibrary.wiley.com/store/10.1029/2006RG000213/asset/equation/rog1654-math-0003.gif?v=1&t=ippj8s7t&s=060425d355ced8d7b10839d0ee943b43171d0166
is the absolute velocity.
Figure 1.
Rotating Earth and the components
Mii
i of the global angular momentum M in the rotating coordinate system with basic vectors i
i. The position vector r points to a volume element
dV in space, where the unit vectors e
λ, eϕ, and e
r of the local rotating spherical coordinate system are defined.
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Figure 2
Time and zonal mean of the (a) axial wind term [
w3] in 106 Had s and (b) south-north difference of the mass term [
m3] in 105 Had s as a function of height
z (km) and latitude. The terms are integrated over zonal annuli of 5° width and 1000 m depth. Data basis is ERA-40 (1958–2001).-----------------------------------------------------------------------
[6] The laws of angular momentum emerged only slowly in fluid mechanics (see
Truesdell [1968] for a lucid account).
Bernoulli [1747] may have been first to apply angular momentum concepts correctly in a model of the equatorial easterlies. On the other hand,
Hadley [1735]used inaccurate arguments concerning angular momentum in his celebrated treatise on trade winds. A historic account is, however, beyond the scope of this article. For our purpose it is sufficient to state that the axial angular momentum cycle of the atmosphere and its link to the rotating Earth via the torques have been a key topic of meteorology at least since the 1950s.
Starr [1948],
Starr and White [1951],
Lorenz [1967], and others worked out the basic features of the atmosphere's axial angular momentum budget (see
Oort [1989] and
Rosen[1993] for introductions into historical aspects). The review by
Oort and Peixoto [1983]describes the mean distribution of the axial angular momentum in the atmosphere, its transports, with particular emphasis on the role of eddies, and the contributions of latitude belts to friction and mountain torques. In general, good agreement is found between observed changes of
M3 and those of LOD as predicted by
(15) [
Rosen, 1993].