Abstract
XBT data, collected in the central North Pacific under the NORPAX program (TRANSPAC) is analyzed , by means of inverse methods (cross-spectral fit). The data are separated into two parts: a fluctuation with length scales in the order of the dimensions of the North Pacific basin and a wavelike fluctation with much shorter scales of a few hundred kilometers. At the annual frequency the wavelike fluctuation is found to consist of a random field of first-order baroclinic Rossby waves travelling basically northwest with wave-lengths of 300 km and phase speeds of 1 cm sSUB- SUB1 . The group velocity is directed mainly southwest and is of the order of 1 cm sSUB-SUB1. The fields of temperature, pressure, velocity, sea level elevation, and horizontal and vertical particle displacement associated with the annual baroclinic Rossby waves are described. (A)
Cite
CITATION STYLE
Kang, Y. Q., & Magaard, L. (1980). Annual baroclinic Rossby waves in the central North Pacific. J. PHYS. OCEANOGR., 10(8, Aug. 1980), 1159–1167. https://doi.org/10.1175/1520-0485(1980)010<1159:abrwit>2.0.co;2
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.