  We demonstrate that the recent measurement of azimuthally collimated, long
range rapidity ("ridge") correlations in $\sqrt{s}=13$ TeV proton-proton (p+p)
collisions by the ATLAS collaboration at the LHC are in agreement with
expectations from the color glass condensate effective theory of high energy
QCD. The observation that the integrated near side yield as a function of
multiplicity is independent of collision energy is a natural consequence of the
fact that multiparticle production is driven by a single semi-hard saturation
scale in the color glass condensate framework. We argue further that the
azimuthal structure of these recent ATLAS ridge measurements strongly constrain
hydrodynamic interpretations of such correlations in high multiplicity p+p
collisions.
