Critical-level behaviour and wave amplification of a gravity wave incident upon a shear layer

THE PROPERTIES OF REFLEXION, REFRACTION AND ABSORPTION OF A GRAVITY WAVE INCIDENT UPON A SHEAR LAYER ARE INVESTIGATED.IT IS SHOWN THAT ONE MUST EXPECT THESE PROPERTIES TO BE VERY DIFFERENT DEPENDING UPON THE PARAMETERS (SUCH AS THE RICHARDSON NUMBER RI, THE WAVELENGTH NORMALIZED BY THE LENGTH SCALE OF THE SHEAR AND THE RATIO OF THE FLOW SPEED TO THE PHASE SPEED OF THE WAVE) CHARACTERIZING THE INTERACTION OF A GRAVITY WAVE WITH A SHEAR LAYER.IN PARTICULAR IT IS SHOWN THAT FOR ALL RICHARDSON NUMBERS THERE IS A DISCONTINUITY IN THE NET WAVE-ACTION FLUX ACROSS THE CRITICAL LEVEL, I.E.AT THE HEIGHT WHERE THE FLOW SPEED MATCHES THE HORIZONTAL PHASE SPEED OF THE WAVE.WHEN RI = 1/4, THIS IS ACCOMPANIED BY ABSORPTION OF PART OF THE ENERGY OF THE INCIDENT WAVE INTO THE MEAN FLOW.IN ADDITION IT IS SHOWN THAT THE PHENOMENON OF WAVE AMPLIFICATION (OVER-REFLEXION) CAN ARISE PROVIDED THAT THE ULTIMATE SHEAR FLOW SPEED EXCEEDS THE HORIZONTAL PHASE SPEED OF THE WAVE AND RI IS LESS THAN A CERTAIN CRITICAL VALUE RI/SUB C/ # 0.1129, IN WHICH CASE THE REFLECTED WAVE EXTRACTS ENERGY FROM THE STREAMING MOTION.IT IS ALSO POINTED OUT THAT WAVE AMPLIFICATION CAN LEAD TO INSTABILITY IF THE BOUNDARY CONDITIONS ARE ALTERED IN SUCH A WAY THAT THE SYSTEM CAN BEHAVE LIKE AN 'AMPLIFIER'.(A.)