1.
Trifunac, M.
D. (1997): Stresses and intermediate frequencies of strong earthquake acceleration. Geofizika, 14, 1-27.
ABSTRACT:
The peak of smooth Fourier amplitude spectra, ((FS(T))max, of strong motion acceleration recorded in California is modelled via dimensional analysis. In this model, the spectrum amplitudes are proportional to (1) the root-mean-square (r.m.s.) amplitude of the peak stresses on the fault surface in the areas of high stress concentration (asperities), and (2) (log10N)1/2, where N is the number of contributing (sampled) asperities. The results imply simple, one asperity, earthquake events for M ≤ 5, and multiple asperity events for M ≥ 5 (N ~ 10 near M = 7and N ~ 100 near M ~ 8). The r.m.s. value of the peak stress drop on the fault, , appears to increase with magnitude for M ≤ 6, and then it levels off near 100 bars, for M ≥ 6. For M < 6, ((FS(T))max continues to grow with magnitude, because of the larger number of asperities from which the sample is taken (N ~ 100 for M = 8), not because of increasing
Keywords : Strong earthquake acceleration, earthquake stress
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2.
Brzović, N. and V. Jurčec
(1997): Numerical simulation of the Adriatic cyclone development. Geofizika, 14,
29-46.
ABSTRACT:
This paper represents
the first attempt to simulate the influence of the
Keywords: Numerical simulation, cyclone development, Adriatic cyclone, influence of orography
[PDF]
3.
Penzar,
ABSTRACT:
The paper deals with weather and
climate descriptions originating before the establishment of the meteorological
station network. The oldest of them stem from as long ago as the second and the
first century B.C. They may be found in local and foreign almanacs, reports,
letters, newspapers and books. In the first part of the paper records of
weather are ordered chronologically. These are casual notes, accounts of
somehow peculiar weather events, and even regular, almost daily weather notes
written through many years in the 18th century in Makarska.
The second segment presents reports on common weather characteristics, i.e.
climate attributes. These are mostly wind accounts, particularly of Bura (Bora), but there are also a
few climatographies.
Keywords: Old meteorological notes, Weather, Climate, the
[PDF]
4.
Tiwari, R. K., J. G. Negi
and K. N. N. Rao (1997): Detection of long term
modulation orbital cycles in the sea level oscillations using clean algorithm
of spectral analysis. Geofizika,
14, 133-147.
ABSTRACT:
The need for a unified astronomical theory of sea-level changes and
associated climatic variations motivates the search for Milankovich
eccentricity rhythms in the global sea level variations. The available latest
sea level record exhibits long term trend with superimposed higher order
frequency oscillations. A new powerful spectral technique based on the one
dimensional clean deconvolution algorithm, is applied
to the global sea level fluctuations record of the past 30 million years. The
spectrum analysis reveals statistically significant (at 90% confidence level)
and “clean” cyclicity of 2000 kyr, 1250 kyr, 880 kry, 660 kyr, 416 kyr, and 260 kry. Statistically
significant sea level cycles indicate possible link with climate and orbital
cycles. A principal cycle (Ep) of 413 kyr
corresponds to the well known orbital eccentricity cycle. The remaining higher
order periodicities are integral multiples of Ep (e.g., Ep/2, 3Ep/2, 2Ep,
3Ep, 5Ep,), equivalent to those of the modulation of orbital eccentricity-precession
cycles. Matching periodicities of the sea level changes and climatic rhythms,
and long term modulation of orbital variations demonstrate significant role of
orbital cycles in these processes and integrate the Milankovich
paradigm of orbital forcing to coupled climate-sea
level interactions.
Keywords: Sea
level oscillations, spectral analysis, clean algorithm
[PDF]
5.
Orlić, M. (1997): The
ABSTRACT:
The activity of
Keywords: Josip Goldberg, research at the
[PDF]
6.
Vilibić,
ABSTRACT:
A brief review is given of recent works
on relative mean sea level, global sea level rising effect and the predictions
to year 2100. The influence of vertical crustal
movements to relative sea level is visible on the longest sea level records.
Both modern space geodetic techniques and absolute gravity measurements have
now achieved the accuracy within a centimeter that is compatible with the above
quality of mean sea level. The extraction of land movements from the tide gauge
record is possible within a decade, so the number of international project have
been (etc. SELF) and will be (etc. MedGLOSS) launched
with the aim to achieve the absolute sea level.
Keywords: Sea level, global sea level rise, GPS,
absolute gravimetry
[PDF]