The dominant weather circulation is determined at 260°.
Solids circulation was determined from the downward velocity of particles in the annulus.
The rapidity of circulation is determined by the output of the heart, which in turn is responsive to overall body requirements.
Each component is represented by vortex lattice lifting lines and the radial distribution of circulation is determined by the solution of the problem.
Consequently, the quantity of domestic currency in circulation is determined solely by market forces, namely the demand for domestic currency.
Edmund Halley, a contemporary of Isaac Newton and still widely known for predicting the periodicity of a comet, first suggested that global atmospheric circulation was determined by temperature gradients (Halley 1686).
The PEEP level (8 cmH2O) that did not induce lung overdistension or compromise circulation was determined.
Leakage of FITC-labeled dextran into the circulation was determined by measurement of the plasma fluorescence (λex/ λem = 488/520 nm).
The uniform quality of air circulation is determined by measuring the differences in temperature, for instance, in distinct zones inside the cold chamber itself.
Duration of MBP circulation was determined by time frame, MBP strain, and lytic activity of the MBP, but not by dose of MBP on the surface.
