- Page 1 and 2: AN ABSTRACT OF THE THESIS OF Roger
- Page 3: Observations and Modelling of Front
- Page 7 and 8: This research was supported by ONR
- Page 9 and 10: TABLE OF CONTENTS I. INTRODUCTION 1
- Page 11 and 12: Figure LIST OF FIGURES (continued)
- Page 13 and 14: OBSERVATIONS AND MODELLING OF FRONT
- Page 15 and 16: II. TOWED THERMISTOR CHAIN OBSERVAT
- Page 17 and 18: oriented multiple surface fronts up
- Page 19 and 20: gravity waves. A maximum of 21 and
- Page 21 and 22: small, since the large-scale temper
- Page 23 and 24: front at about 18.5 °C. There is f
- Page 25 and 26: given in the stable cases (downward
- Page 27 and 28: temperatures for January and Februa
- Page 29 and 30: dominates the spectrum. At these wa
- Page 31 and 32: typically iO-2iO3 °c m1-), and sin
- Page 33 and 34: 11.5 Geostrophic turbulence We have
- Page 35 and 36: energy of each of the longitudinal
- Page 37 and 38: varying N and a flow isolated from
- Page 39 and 40: adiabatic meridional displacements
- Page 41 and 42: z0 34 32 V v 30 a -J 28 26 a) - 2b$
- Page 43 and 44: U0 V L 0 L V 20 E 16 V 12 p ; t *,
- Page 45 and 46: 30 E 50 -c a- I, 0 70 90 300 360 37
- Page 47 and 48: 10 10° 10-2 1 0 -3.0 -2.0 -1.0 0.0
- Page 49 and 50: 1 o 1 102 101 - 0 LU 00 x I.- - -1
- Page 51 and 52: E (I) a. z 106 1 o5 102 101 100 1O
- Page 53 and 54: Table 11.1 Tow start and finish pos
- Page 55 and 56:
Table 11.3 Climatological sea surfa
- Page 57 and 58:
Paulson, C. A., R. J. Baumann, L. M
- Page 59 and 60:
111.1 Introduction In this chapter
- Page 61 and 62:
interior layers, on the horizontal
- Page 63 and 64:
polynomials in z.) The vertical mom
- Page 65 and 66:
hit + (hivi) = We, (8a) h2t + (h2v2
- Page 67 and 68:
Equations (la) and (2a) are dynamic
- Page 69 and 70:
subdivided into subdomains with dif
- Page 71 and 72:
mixed layer. As is the case with (2
- Page 73 and 74:
constant pressure c = 4.1x103 J K1-
- Page 75 and 76:
When (28) have been solved for the
- Page 77 and 78:
occur with the initial conditions w
- Page 79 and 80:
analytically. Let Al2 and A23 be th
- Page 81 and 82:
Shortly after t = 8.1, the mixed la
- Page 83 and 84:
that around the offshore front, exc
- Page 85 and 86:
the reduced equations numerically.
- Page 87 and 88:
(1) The upwelled horizontal profile
- Page 89 and 90:
Figure 111.1 Model geometry. zO z z
- Page 91 and 92:
* j 0. -20. >\ - -40. 0 > .0 0. 40.
- Page 93 and 94:
4) 20. 10. 0. 20. 1 0. 0. 0 y/X 0.
- Page 95 and 96:
BIBLIOGRAPHY Batchelor, G. K. , 195
- Page 97 and 98:
Rhines, P. B., 1979: Geostrophic Tu
- Page 99 and 100:
APPENDIX A: DYNAMICAL DERIVATION OF
- Page 101 and 102:
In a manner exactly analogous to th
- Page 103 and 104:
smoothness. The large vorticities t