BUKU BASA PORTUGIS KAKAIT KARO «COTIDAL»
Temukaké kagunané saka
cotidal ing pilihan bibliografi iki. Buku kang kakait dening
cotidal lan pethikan cekak kang padha kanggo nyediyakaké panggunané ing sastra Basa Portugis.
There are, however, in these statements, certain errors and imperfections, which
prevent our being able as yet to determine the course of the cotidal lines with
accu_racy, or even to obtain with certainty a first approximation to these lines.
2
Approximate
Cotidal Lines of Diurnal and Semi-diurnal Tides ...
The agreement of the cotidal hours as computed and observed is less
satisfactory in the larger groups than in the smaller ones as might be expected.
On the map No. 5, a rough outline of the Gulf' Coast is traced, and the cotidal
hours are ...
Alexander Dallas Bache, 1857
3
Bulletin of the National Research Council
tailed explanation of tides is very incomplete, and attention has been largely
given in the past to the geographical distribution, usually described by cotidal
lines, and utilizing actual observations on the coasts. It will be recalled that a
cotidal line ...
two cotidal maps, one for the British Isles and the other for the world at large
between the latitudes 60° N. and 52° S. In the latter of these maps the cotidal
lines are drawn across the wide expanses of the Atlantic and Indian Oceans from
shore ...
5
The American Journal of Science
cotidal line with the meridian N.'35° 30' W. and the mean cotidal hour 18b 50"',
the difference of establishment for one geographical mile perpendicular to the
cotidal line 4-7 minutes. As the observations at Santa Cruz were comparatively
few ...
6
Report of the Superintendent of the (United States) Coast ...
M^ + N Ixy = Ixz M 2" x y -f- N S y2 = 1' y z In the case before us, M gives for the co
-efficient of the longitude 1.2, and N for that of lati- N 1ude =0.006. The tangent of
the an j;le which the cotidal line makes with the meridian — = 0.05, and the ...
7
The American Journal of Science and Arts
cotidal line with the meridian N. 35° 30' W. and the mean co- tidal hour 18b 50m,
the difference of establishment for one geographical mile perpendicular to the
cotidal line 4-7 minutes. As the observations at Santa Cruz were comparatively
few ...
8
On the Tides of the Atlantic and Pacific Coasts of the ...
cotidal line with the meridian N. 35° 30' W. and the mean co- tidal hour 18b 60m,
the difference of establishment for one geographical mile perpendicular to the
cotidal line 47 minutes. As the observations at Santa Cruz were comparatively
few ...
Alexander Dallas Bache, 1856
9
Basic Wave Mechanics: For Coastal and Ocean Engineers
Cotidal lines, which are lines connecting points that have a maximum surface
elevation at the same instant, can be determined from Eq. 9.24. Maximum surface
elevation occurs when at = 0 or e~/y/c sin(fcc - at) + efy/c sin(fct + at) = 0 which, ...
10
Encyclopedia of Marine Science
The pattern of the tide is shown by plotting cotidal lines, or isolines of equal
phase of the tide wave around the amphidromic point. The cotidal lines can be
labeled with degrees of phase, or in time intervals in hours, of either solar time or
lunar ...
C. Reid Nichols, Robert G. Williams, 2009
BABAGAN WARTA KANG NGLEBOKAKÉ ARAN «COTIDAL»
Weruhi yèn pawarta nasional lan internasional wis ngomongaké lan kepriyé aran
cotidal digunakaké ing babagan warta iki.
In Chile, Turbulence Ahead
In the 19th century, William Whewell mobilized the global British empire to gather data for the first “cotidal” charts, only to find that local phenomena often ... «New York Times, Jan 13»
