January 2010
·
6 Reads
·
2 Citations
This page lists works of an author who doesn't have a ResearchGate profile or hasn't added the works to their profile yet. It is automatically generated from public (personal) data to further our legitimate goal of comprehensive and accurate scientific recordkeeping. If you are this author and want this page removed, please let us know.
January 2010
·
6 Reads
·
2 Citations
January 2010
·
9 Reads
January 2010
·
13 Reads
January 2010
·
16 Reads
·
4 Citations
January 2010
·
10 Reads
January 2010
·
3 Reads
·
1 Citation
January 1999
·
15 Reads
·
5 Citations
January 1998
·
42 Reads
·
5 Citations
November 1992
·
12 Reads
·
1 Citation
An experimental voice command and integrated navigation system is described. The implementation is in a Convair 580 research aircraft. The system uses an interactive cockpit display to provide waypoint and routing management, fuel information, aircraft positioning, and navigation information and flight planning functions. For in situ measurement of physical phenomena, steering information is provided on cockpit course deviation indicators from flight guidance software. These functions are integrated together with a Macrospeak voice recognizer, so that voice commands can be used to control the system from the cockpit. The design of the system is discussed, considering the specialized role of the aircraft, including the various design tradeoffs made. The system was used operationally in its present form during recent field experiments including a magnetic survey over the Arctic Ocean
February 1992
·
19 Reads
·
18 Citations
Geophysics
A new technique has been developed to estimate the vertical magnetic gradient (Gz) along a profile from measurements of the two orthogonal horizontal magnetic gradients (Gx and Gy). In addition, a means of identifying two-dimensional anomaly sources and the angle of the structure relative to the profile direction is shown to be a function of θ = arctan (-Gy/Gx). This angle can be used to correct interpretations from vertical gradient or total field inversion methods which assume source structures oriented perpendicular to the profile direction. A modified Werner deconvolution algorithm for vertical gradient data incorporating these features has been applied to both real and simulated horizontal gradient data.
... Conversely, measurements of the vertical and horizontal magnetic gradients have significant advantages over total magnetic field surveys with single-sensor magnetometry. These include the reductions in regional magnetic gradients, the elimination of short-term diurnal fluctuations, and the attenuation of longer wavelength anomalies due to deeper magnetic sources; thus, smaller-scale shallow anomalies are enhanced by removing the masking effects of longer wavelength anomalies (Young and Droege [42]; Marcotte et al. [78]), improving the resolution of minor anomalies, and resolving complex anomalies (Cowan et al. [79]). Another advantage of using a gradiometer is that the transient signals of the Earth's magnetic field are the same for the two sensors, so it completely cancels out any differences in signals that are unaffected by diurnal variations (Sharma [60]; Mussett and Khan [68]; Milsom and Eriksen [76]; Cowan et al. [79]). ...
February 1992
Geophysics
... Methods that enhance trends are particularly important, and several techniques have been put forward to enhance trends in aeromagnetic maps. Using measured gradients can dramatically improve the trend of sharp features and/or linear structures at an acute angle with respect to flight lines (Marcotte et al., 1990;Cowan et al., 1995;McMullan et al., 1995;Hardwick, 1999;O'Connell et al., 2005;Reford, 2006). Yunxuan (1993) uses a band-limited Radon transform (RT) as applied to synthetic gravity maps to remove boudinage artifacts, but the technique remains limited to only one trend direction. ...
January 1999
... No clear pattern of sea-floor spreading anomalies has yet been observed, partly because data distribution and quality are insufficient. An aeromagnetic survey program has been initiated over the Canadian polar continental margins (Nelson et al. 1991), but more data are needed on a regional scale. Given present and foreseeable technology, a regional airborne mapping program covering the entire Amerasian Basin appears to be an effective means to acquire that data. ...
January 2010
... These yields detailed data about shallow geological characteristics, which remain unaltered by diurnal fluctuations and the magnetic field background of the region. As an illustration of the gradient tensor measurement's power, the Canadian Geological Survey initiated an aeromagnetic gradiometer program in Canada, developing short baseline aeromagnetic gradiometers back in 1975 [30][31][32]. ...
January 1992
Journal of geomagnetism and geoelectricity
... The objective of the project is to achieve a regional, aeromagnetic coverage of the Greenland ice cap, and to produce magnetic anomaly maps for use in research on the large scale geological structures. Field work was carried out in 1983, 1984(Thorning et al. , 1984,1986. The work reported in this note was originally planned for April 1986, but for technical reasons it had to be postponed until April 1987. ...
December 1984
Grønlands Geologiske Undersøgelse Rapport
... The magnetic anomaly pattern over North Greenland and the adjacent Lincoln Sea bears many similarities with the magnetic anomalies of the Yelverton Bay area (Damaske et al., 1997;Nelson et al., 1998;Damaske & Estrada, 2006;. A broad magnetic high over the southern Lincoln Sea (Damaske & Estrada, 2006, fig. 3) is comparable with the magnetic high H1 over Yelverton Bay. ...
January 1998
... It does not require storage of historical data and offers a high real-time advantage, with an exceptional filtering effect especially in the transient state of initial filtering. The Kalman filter was originally designed and developed for aircraft navigation [14]. It is used mainly to estimate the system state that can be observed only indirectly or imprecisely. ...
June 1991