Fróðskaparrit - 01.01.1975, Síða 84

92
Sea Level Fluctuations in Tórshavn, Preliminary Results
TABLE IV Harmonic constants for Torshavn. The Greenwich Phase lag is the
lag of the constituent relative to the phase of the relevant component of
the astronomic đriving force measured at Greenwich. The local time lag is
the time that the constituent lags behind (in case of minus : leads) the
driving force. Amplitude and phaselag have been corrected for nodular mo-
dulation.(ADD.LAG : Additional lag, GR.P.LAG : Greenwich Phase Lag,
L. T. LAG : Lo c: a 1 Ti. me Lag)
SYMBOL DOODSON NO. iQj oVoVo ADD;LAG deg. FREQUENCY c/h PERIOD h AMPLIT; cm GR.P.LAG deg. L.T h LAG min
Ssa 0 0 2 0 0 0 180 .000228 4386 6.31 85 1033
H cy 1-2 0 1 0 0 -90 .037219 26.87 2.57 22 1 9
1-1 0 0 0 0 -90 .038731 25.82 9.98 57 3 37
N0± 10 0 1 0 0 90 .040269 24. 83 .91 -21 -1 53
L 1 1-2 0 0 0 -90 .041553 24.07 1.36 116 7 17
Ki 110 0 0 0 90 .041781 23.93 4.84 130 8 12
2MS7 2-2 2 0 0 0 0 .077689 12.87 .47 87 2 38
u2 2-1 0 1 0 0 0 .078999 12.66 1.79 175 5 40
»2 2 0 0 0 0 0 •o .080511 12.42 9.89 -164 -6 8
2MN9 2 10 1 0 0 0 .082024 12.19 .65 53 1 20
S2 2 2-2 0 0 0 0 .083333 12.00 5.81 -134 -4 55
k2 2 2 0 0 0 0 0 .083561 11.97 2.13 -161 -5 48
M3 3 0 0 0 0 0 180 .120767 8.28 .62 111 2 5
mk3 3 10 0 0 0 90 .122292 8.18 .40 -16 3 -4 10
MN 4-1 0 1 0 0 0 .159511 6.27 1.30 -85 -1 57
M4 4 0 0 0 0 0 0 .161023 6.21 2.81 -56 -1 26
MS„ 4 2-2 0 0 0 o .163845 6.10 2.16 -32 -1 1
2MK6 6-1 0 1 0 0 0 .240022 4.17 .81 167 1 28
M6 6 0 0 0 0 0 0 .241534 4.14 1.31 -148 -2 11'
msn6 6 1-2 1 0 0 0 .242844 4.12 .66 -138 -2 2
2MS6 6 2-2 0 0 0 0 .244356 4.09 1.55 -102 -1 37
4MS10 10 2-2 0 0 0 0 .405379 2.47 .35 -85 -1 . 3
3MS.n 10 4-4 0 0 0 0 .408201 2.45 .43 -75 -0 58
TALVA IV. Aldingar í flóðini í Havn. Fyrstu trý røðini vísa almenn
nøvn og eyðkenni, fjórða rað: Títtleikan (aldingar í tíman), fimta rað:
Aldutíðina (í tímum), sætta rað: Styrkina (í cm), sjeynda rað: Seinkingina
av aldingini í mun til sól og mána roknað í gradum og frá Greenwich og
áttanda rað vísir seinkingina roknaða í tímum frá Havnini (— svarar til
at aldingin er komin framum).
Meteorological influence Having determined — to a certain
degree — the astronomic tide, this may be subtracted from the
original time series. Referring to the resulting series as »Reduced
water level« we may investigate to what degree this series is
of meteorological origin.
In fig. 6 is shown the PDS of reduced water level and in