204 Dynamics of Atmospheres and Oceans, 6 (1982) 204 Elsevier Scientific Publishing Company, Amsterdam -- Printed in The Netherlands

Errata

Wang, C.S. and Street, R . L , 1978. Measurements of spray at an air--water interface. Dyn. Atmos. Oceans, 2: 141--152.

page 141, Abstract, line 10, u.o/v ~ 0.3, should read: u.o/v ~ 300.

page 148, Fig. 5, abscissa, should read: U.Zod/V (× 10-4);

ordinate, should read: u.a/v (× 10-3);

U*Z°d-1.9(U*J~ - -0 .6 , should read: U*Z°d-19.4(U*Ot - - 6 0 0 0 . O ~ O ] O ~ u /

page 151, Equation 14, should read: Rd = 1 9 . 4 R o - - 6 0 0 0 .

page 152, Acknowledgment, add: The authors are indebted to Dr. Y. Sinai, National

Nuclear Corp. Ltd., England, for bringing the lost powers of 10 to their attention.

Corrigenda

Welander, P., 1981. A note on the overall vorticity balance in w ind , r i ven ocean circulation. Dyn. Atmos. Oceans, 6: 125--130. page 127,

section 3, line 7, equation should read:

b/2 b

f fU dy + f fU dy = 1/p ffcurl ~-~ dA < 0. 0 b/2 A'

page 128, section 4, paragraph 2, lines 4--11, should read: In this case one finds, by

scalar multiplication of the vector vorticity equation Dq/Dt = (q • V ) v -- V (1/p) × V p + curl F by V p, (q = 2 ~ + curl v, F the friction force), that

DP/Dt = q • VQd + Vp • curl F (7)

where P = q • V p is the potential vorticity in the incompressible approxima- tion. The right-hand side can be written V • (qQd + F × Vp), and integrating over an ocean with fixed boundaries (a rigid lid at the top), we have

ff + F X Vp) dA = O (8) A