8 research outputs found
Late mortality and causes of death among 5-year survivors of childhood cancer diagnosed in the period 1960–1999 and registered in the Italian Off-Therapy Registry
The boundary value problem approach to the data reduction for a spaceborne gradiometer mission
DEM Generation with digital photogrammetry and laser scanning in architectural structures survey
The observation equation of spirit leveling in Molodensky's context
Spirit leveling and surface gravity observations can be expressed as orthometric height
differences plus corrections which require the knowledge of the Earth crust density. For
leveling increments we can write observation equations in a linearized form, according
to the standard Molodensky approach, i.e., intrinsic geodesy, depending on normal height
differences plus a correction term. This term is a function of the gravity anomaly at the
surface level, thus not requiring any assumption on the crust density, and of the curvature of
the normal field force lines, which can not be neglected for leveling profiles directed along
meridians. The present work shows how to derive these observation equations. An example
is presented to verify the effectiveness of the new approach
Orthometric correction and normal heights for Italian levelling network: a case study
Levelling increments must be corrected for gravity
in order to get proper dynamic or orthometric heights. In Italy,
most of the levelling lines have no associated gravity observations.
Thus, only levelling increments are available, and
corrections were computed only on a subset of the existing
lines. However, gravity is densely observed, and thus, predictions
of gravity along the levelling lines can be computed.
This, in principle, would allow the estimation of corrections
along the whole Italian levelling network. Furthermore, global
model-derived gravity could be used for the same task (e.g.
one could use the EGM2008 global geopotential model to get
gravity estimates). To check for the reliability of these procedures,
a test has been performed along levelling lines in the
western Alps area. Both dynamic and orthometric corrections
have been computed in order to finally get geopotential numbers,
normal heights and orthometric heights from raw levelling
increments. The results proved that reliable results can be
obtained using the Italian gravity database, while predictions
based on the EGM2008 model led to poorer estimates