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Although airborne gravimetry is now considered a fully operational technique, errors due to motion compensation using differential
GPS (DGPS) continue to influence both its accuracy and the range of applications in which it can be used. In typical medium-resolution
applications such as airborne geoid mapping, errors due to DGPS contribute considerably to the error budget of an airborne
gravity system. At the same time, efforts to increase the resolution of such systems for demanding applications such as resource
exploration remain impedded by errors in DGPS.
This article has three objectives. The first one is to compare eight industrially relevant DGPS software packages for the
determination of aircraft acceleration. The second objective is to analyze and quantify the effect that each relevant portion
of the DGPS error budget has on the determination of acceleration. Using data sets that represent a wide range of operational
conditions, this is done in the frequency domain over a range of frequencies corresponding to spatial resolution as high as
450 m. The third objective is to use that information to recommend and demonstrate approaches that optimize the estimation
of aircraft acceleration for determining the geoid and for resource exploration.
It is shown, for example, that the time of day in which the survey is carried out and the dynamic characteristics of the aircraft
being used are two of the most crucial parameters for very high-resolution gravity field estimation. It is demonstrated that
when following the above-mentioned recommendations, agreements with ground daa of better than 1.5 and 2.5 mGal can be achieved
for spatial resolutions (half-wavelengths) of 2.0 and 1.4 km, respectively. ? 2002 Wiley Periodicals, Inc. 相似文献
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Accurate estimates of the velocity and acceleration of a platform are often needed in high dynamic positioning, airborne gravimetry,
and geophysics. In turn, differentiation of GPS signals is a crucial process for obtaining these estimates. It is important
in the measurement domain where, for example, the phase measurements are used along with their instantaneous derivative (Doppler)
to estimate position and velocity. It is also important in postprocessing, where acceleration is usually estimated by differentiating
estimates of position and velocity. Various methods of differentiating a signal can have very different effects on the resulting
derivative, and their suitability varies from situation to situation. These comments set the stage for the investigations
in this article. The objective is twofold: (1) to carry out a comprehensive study of possible differentiation methods, characterizing
each in the frequency domain; and (2) to use real data to demonstrate each of these methods in both of the measurement and
position domains, in conditions of variable, high, or unknown dynamics. Examples are given using real GPS data in both the
measurement domain and in the position and velocity domain. The appropriate differentiator is used in several cases of varying
dynamics to derive a Doppler signal from carrier phase measurements (rather than using the raw Doppler generated by the receiver).
In the statistic case, it is seen that the accuracy of velocity estimates can be improved from 4.0 mm/s to 0.7 mm/s by using
the correct filter. In conditions of medium dynamics experienced in an airborne gravity survey, it is demonstrated that accelerations
as the 2–4 mGal level (1 mGal = 0.00001 m/s2) can be obtained at the required filtering periods. Finally, a precision motion table is used to show that when using the
correct filter, velocity estimates under high dynamics can be improved by an order of magnitude to 27.0 mm/s. ? 1999 John
Wiley & Sons, Inc. 相似文献
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New and important roles for DMSP in marine microbial communities 总被引：4，自引：0，他引：4
The algal osmolyte dimethylsulfoniopropionate (DMSP) is recognised as the major precursor of marine dimethylsulfide (DMS), a volatile sulfur compound that affects atmospheric chemistry and global climate. Recent studies, using 35S-DMSP tracer techniques, suggest that DMSP may play additional very important roles in the microbial ecology and biogeochemistry of the surface ocean. DMSP may serve as an intracellular osmolyte in bacteria that take up phytoplankton-derived DMSP from seawater. In addition, DMSP appears to support from 1 to 13% of the bacterial carbon demand in surface waters, making it one of the most significant single substrates for bacterioplankton so far identified. Furthermore, the sulfur from DMSP is efficiently incorporated into bacterial proteins (mostly into methionine) and DMSP appears to be a major source of sulfur for marine bacterioplankton. Assimilatory metabolism of DMSP is via methanethiol (MeSH) that is produced by a demethylation/demethiolation pathway which dominates DMSP degradation in situ. Based on the linkage between assimilatory metabolism of DMSP and bacterial growth, we offer a hypothesis whereby DMSP availability to bacteria controls the production of DMS by the competing DMSP lyase pathway. Also linked with the assimilatory metabolism of DMSP is the production of excess MeSH which, if not assimilated into protein, reacts to form dissolved non-volatile compounds. These include sulfate and DOM–metal–MeSH complexes, both of which represent major short-term end-products of DMSP degradation. Because production rates of MeSH in seawater are high (3–90 nM d−1), reaction of MeSH with trace metals could affect metal availability and chemistry in seawater. Overall, results of recent studies provide evidence that DMSP plays important roles in the carbon, sulfur and perhaps metal and DOM cycles in marine microbial communities. These findings, coupled with the fact that the small fraction of DMSP converted to DMS may influence atmospheric chemistry and climate dynamics, draws attention to DMSP as a molecule of central importance to marine biogeochemical and ecological processes. 相似文献
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J. R. Bruton D. S. Hall L. J. Boyd R. M. Genet R. D. Lines H. C. Lines C. D. Scarfe 《Astrophysics and Space Science》1989,155(1):27-38
HD 165590 is a visual binary (dG0 + dG5,P = 20
.
y
25,e = 0.96) whoseA component is an SB1 double (dG5 + dM:P = 0
.
d
88,e0.0). TheA pair (Aa +Ab) undergoes partial eclipses. PhotoelectricUBV photometry from Lines and one of the Automatic Photoelectric Telescopes, andV photometry from Scarfe are examined here. The data are from the 1977, 1984, 1985, and 1986 observing seasons. The non-eclipse light variations are analyzed with a FORTRAN program which does a sinusoidal curve fitvia least squares repeatedly to obtain the best period. Periods found from each observing season and passband are consistent with Boydet al. (1985): the greatest variations seem to be produced by a rotating (0
.
d
88), spotted, G0 star (theAa component). To the residuals from the first analysis a further curve fit is made to determine characteristics of the wave due to the ellipticity effect. An early limit on the spectral type of the unseenAb component, based on the primary eclpse depth and the upper limit on the depth of the unseen secondary eclipse, is K2. Eclipse depths and widths seen here suggest that theA pair's inclination = 74
.
0
9 ± 10, close to theA +B inclination of 82
.
0
7 ± 20 (Battenet al., 1979). TheA pair's orbital period does not appear to vary, appearing instead to be well-described by a new linear ephemeris (Hel. J.D. = 2443665.4568 + 0
.
d
8795045E) which does, however, take into account a variable light-travel-times as theA component orbits theA +B center of mass with a 20
.
y
25 period. The maximum light-travel-time O-C thus produced is + /–8
.
m
4 = + /–0
.
d
0059. 相似文献
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Ordovician faunal data from the Scandinavian Caledonides is tested with new geochemical information from zircons to give U/Pb ages and source origins of volcanic arc and ophiolite sequences. Early Ordovician (Arenig-Llanvirn), low latitude, Toquima-Table Head faunas from the upper Upper Allochthon are associated with an island arc system formed adjacent to Laurentia. Contemporaneous mafic magmas were contaminated by crustal material during subduction and associated granites contain inherited zircons of Archaean age. The nearest source for such rocks is on the Laurentian rather than the Baltic side. Higher latitude Celtic province faunas from the upper Upper Allochthon are from one insular site accessible to forms from both Laurentia and Baltica.
The late Ordovician low-latitude Holorhynchus and subtropical Hirnantia faunas occur in overstep sequences above deeply eroded early Ordovician arc complexes. The transgression appears to be coeval with a second generation of spreading-related complexes. Single detrital zircons from sediments show sources from Archaean, Proterozoic and early Ordovician terranes. This suggests that deposition was in a basin situated along the same continental margin (Laurentia) to which the early Ordovician ophiolite/arc sequences had already become accreted. The late Ordovician faunas link both Laurentia and Baltica at a time of narrowing of lapetus.
The new geochemical data together with the faunal information is supported by recent palaeomagnetic studies. 相似文献
The late Ordovician low-latitude Holorhynchus and subtropical Hirnantia faunas occur in overstep sequences above deeply eroded early Ordovician arc complexes. The transgression appears to be coeval with a second generation of spreading-related complexes. Single detrital zircons from sediments show sources from Archaean, Proterozoic and early Ordovician terranes. This suggests that deposition was in a basin situated along the same continental margin (Laurentia) to which the early Ordovician ophiolite/arc sequences had already become accreted. The late Ordovician faunas link both Laurentia and Baltica at a time of narrowing of lapetus.
The new geochemical data together with the faunal information is supported by recent palaeomagnetic studies. 相似文献
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A comparison of stable platform and strapdown airborne gravity 总被引：3，自引：1，他引：2
C. L. Glennie K. P. Schwarz A. M. Bruton R. Forsberg A. V. Olesen K. Keller 《Journal of Geodesy》2000,74(5):383-389
To date, operational airborne gravity results have been obtained using either a damped two-axis stable platform gravimeter
system such as the LaCoste and Romberg (LCR) S-model marine gravimeter or a strapdown inertial navigation system (INS), showing
comparable accuracies. In June 1998 three flight tests were undertaken which tested an LCR gravimeter and a strapdown INS
gravity system side by side. To the authors' knowledge, this was the first time such a comparison flight was undertaken. The
flights occurred in Disko Bay, off the west coast of Greenland. Several of the flight lines were partly flown along existing
shipborne gravity profiles to allow for an independent source of comparison of the results. The results and analysis of these
flight tests are presented. The measurement method and error models for both the stable platform and strapdown INS gravity
systems are presented and contrasted. An intercomparison of gravity estimates from both systems is given, along with a comparison
of the individual estimates with existing shipborne gravity profiles. The results of the flight tests show that the gravity
estimates from the two systems agree at the 2–3 mGal level, after the removal of a linear bias. This is near the combined
noise level of the two systems. It appears that a combination of both systems would provide an ideal airborne gravity survey
system, combining the excellent bias stability of the LCR gravimeter with the higher dynamic range and increased spatial resolution
of the strapdown INS.
Received: 3 June 1999 / Accepted: 30 November 1999 相似文献
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