scholarly journals Diurnal cycles of near‐surface currents across the tropical Pacific

Author(s):  
Jessica Masich ◽  
William S. Kessler ◽  
Meghan F. Cronin ◽  
Karen R. Grissom

2019 ◽  
Vol 14 (6) ◽  
pp. 064020 ◽  
Author(s):  
Shirley Leung ◽  
LuAnne Thompson ◽  
Michael J McPhaden ◽  
K A S Mislan


2009 ◽  
Vol 39 (5) ◽  
pp. 1200-1215 ◽  
Author(s):  
Meghan F. Cronin ◽  
William S. Kessler

Abstract Near-surface shear in the Pacific cold tongue front at 2°N, 140°W was measured using a set of five moored current meters between 5 and 25 m for nine months during 2004–05. Mean near-surface currents were strongly westward and only weakly northward (∼3 cm s−1). Mean near-surface shear was primarily westward and, thus, oriented to the left of the southeasterly trades. When the southwestward geostrophic shear was subtracted from the observed shear, the residual ageostrophic currents relative to 25 m were northward and had an Ekman-like spiral, in qualitative agreement with an Ekman model modified for regions with a vertically uniform front. According to this “frontal Ekman” model, the ageostrophic Ekman spiral is forced by the portion of the wind stress that is not balanced by the surface geostrophic shear. Analysis of a composite tropical instability wave (TIW) confirms that ageostrophic shear is minimized when winds blow along the front, and strengthens when winds blow oblique to the front. Furthermore, the magnitude of the near-surface shear, both in the TIW and diurnal composites, was sensitive to near-surface stratification and mixing. A diurnal jet was observed that was on average 12 cm s−1 stronger at 5 m than at 25 m, even though daytime stratification was weak. The resulting Richardson number indicates that turbulent viscosity is larger at night than daytime and decreases with depth. A “generalized Ekman” model is also developed that assumes that viscosity becomes zero below a defined frictional layer. The generalized model reproduces many of the features of the observed mean shear and is valid both in frontal regions and at the equator.



1999 ◽  
Vol 104 (C10) ◽  
pp. 23313-23326 ◽  
Author(s):  
Gary S. E. Lagerloef ◽  
Gary T. Mitchum ◽  
Roger B. Lukas ◽  
Pearn P. Niiler




1996 ◽  
Vol 101 (C2) ◽  
pp. 3629-3647 ◽  
Author(s):  
Claude Frankignoul ◽  
Fabrice Bonjean ◽  
Gilles Reverdin


2001 ◽  
Vol 106 (C8) ◽  
pp. 16673-16684 ◽  
Author(s):  
Semyon A. Grodsky ◽  
James A. Carton


Author(s):  
Judith A. Bennett

Coconuts provided commodities for the West in the form of coconut oil and copra. Once colonial governments established control of the tropical Pacific Islands, they needed revenue so urged European settlers to establish coconut plantations. For some decades most copra came from Indigenous growers. Administrations constantly urged the people to thin old groves and plant new ones like plantations, in grid patterns, regularly spaced and weeded. Local growers were instructed to collect all fallen coconuts for copra from their groves. For half a century, the administrations’ requirements met with Indigenous passive resistance. This paper examines the underlying reasons for this, elucidating Indigenous ecological and social values, based on experiential knowledge, knowledge that clashed with Western scientific values.



1901 ◽  
Vol 35 (412) ◽  
pp. 317-318


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