D. L. Marcotte’s research while affiliated with National Research Council Canada and other places

What is this page?


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.

Publications (51)


Wind and Flux Measurement on NRC Aircraft.
  • Article

January 2010

·

10 Reads

·

B. W. Leach

·

C. D. Hardwick

·

D. Marcotte

yes








Figure 3. Photographs of the Nevzorov Probe mount and camera as used on the NRC-Convair-580 including from left to right: a) photo of roof of aircraft looking forward, b) camera mount inside cabin, and probe mount before installation on aircraft. The distance from the aircraft skin to the probe sensor is 38.4 cm, and the distance from the skin to the light is 49.5 cm.  
Figure 4. The concentration enhancement calculated based on the King (1984) droplet trajectory and air flow model plotted as a function of distance from the fuselage surface of the Convair-580 aircraft and the droplet diameter. The airspeed was assumed to be 100 ms-1. The Nevzorov probe was placed roughly at 0.38 m from the Convair's skin. Particles greater than about 120 µm will be in a shadow zone (shaded area). For the Convair, the shadow zone maximum occurs at a droplet diameter 160 µm. Twohy and Rogers (1993), using more sophisticated models, have shown that much larger particles, with greater inertia, will cross the streamlines and not be shadowed.
Assessing the Collection Efficiency of Natural Cloud Particles Impacting the Nevzorov Total Water Content Probe
  • Article
  • Full-text available

January 2006

·

197 Reads

·

20 Citations

yes

Download

The NRC Atmospheric Research Aircraft

September 2001

·

30 Reads

·

14 Citations

The Flight Research Laboratory of the National Research Council of Canada has an active program of airborne atmospheric research that has been realized primarily in collaboration with other Canadian, as well as American, agencies. The current focus is on global change science, aircraft icing and airborne remote sensing system development. Over the past 50 years, research has been conducted on a diverse array of science and technology issues, driven by contemporary aerospace concerns and, more generally, national and societal needs of the day. The Laboratory's initial efforts in airborne atmospheric science started in 1953, and included work in helicopter icing, work in aircraft structural integrity under turbulent conditions, as well as studies to characterize atmospheric turbulence in general. Presently, projects in the realm of airborne atmospheric science have been organized around the Twin Otter and the Convair 580 aircraft. In recent years, these aircraft have been developed to support research efforts in aircraft icing (Convair 580), air quality and global change science (Twin Otter), as well as remote sensing of the atmosphere and the Earth (both the Convair 580 and the Twin Otter). A particular strength is the precise measurement of atmospheric motion - which, in turn, permits a well-regarded capability in airborne flux measurement (the measurement of the total vertical flow of a quantity of interest, i.e., water vapour or heat). This paper includes brief summaries of the flight envelopes and the instrumentation on-board the Twin Otter and Convair 580 when configured for atmospheric research. The variety and application of the data collected by these aircraft are demonstrated with examples from several recent experiments.


Figure 3. CFDE I (top panel) and CFDE III and AIRS (bottom panel) 300 s (30 km) averaged data plotted against the FAR 25 Appendix C envelopes for 0,-10 and-20 ºC, and the Newton envelopes for light (1 g cm-2 h-1 ), moderate (6 g cm-2 h-1 ) and severe (12 g cm-2 h-1 ) icing. Open symbols represent points that are outside of the FAR 25C envelopes at the corresponding temperature.
Figure 4. A photo of the Convair-580 showing runback ice just aft of the heated leading edge of the wing for the severe icing episode of 16 February over Mirabel at-29ºC. Rime icing can be seen on the forward portion of the wing tip probe.
Table 6 .
Recent Canadian Research on Aircraft In-Flight Icing.

September 2001

·

1,557 Reads

·

105 Citations

A cooperative research program on aircraft in-flight icing, between the National Research Council of Canada and the Meteorological Service of Canada, has been active since the 1950s. Most recently, the Canadian Freezing Drizzle Experiment (CFDE) and the Alliance Icing Research Study (AIRS) were organized to characterize icing environments associated with freezing drizzle; develop better techniques for forecasting such events; and develop our ability to remotely detect icing regions. These field projects, involving instrumented aircraft, were conducted out of Newfoundland (March, 1995) and Ontario (1996/97, 1997/98, and 1999/00). Newfoundland and the Great Lakes are the two regions in North America with the highest frequency of freezing precipitation at the surface. Freezing drizzle, or supercooled large drops (SLD), is considered to be a dangerous icing condition that is not covered by current aircraft certification procedures. The median liquid water contents measured in clouds in both regions were similar, while the droplet concentrations and the frequency of occurrence of mixed phase clouds tended to be higher in Ontario. In both Newfoundland and Ontario, conditions with SLD were often found outside the envelopes used to certify aircraft for inflight icing. Approximately 80% of the SLD environments were assessed to have formed through a non-classical formation mechanism. Forecasting icing conditions remains a challenge. Although new, more physically realistic, in-flight icing forecast schemes have been developed, verification of these forecasts, using the in situ aircraft data, shows that considerable improvement can still be made.


Citations (14)


... Simulations allowed identification of stable features of the inverted fields. Shamsipour et al. (2010b) explored the adaptation of the method to gravity gradients. In this article, we present the 3D inversion of airborne gravity gradient data constrained by geological or physical properties of rocks, using stochastic methods, a practical extension of the work of Shamsipour et al. (2010a, 2010b). ...

Reference:

3D unconstrained and geologically constrained stochastic inversion of airborne vertical gravity gradient data
3D stochastic inversion of borehole and surface gravity data using Geostatistics
  • Citing Conference Paper
  • January 2010

... 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]). ...

Automated interpretation of horizontal magnetic gradient profile data
  • Citing Article
  • February 1992

Geophysics

... Mixed-phase clouds (MPCs) are frequently occurring in the Arctic: they can persist over several days under different meteorological conditions (e.g., Shupe and Intrieri, 2004;Morrison et al., 2012;Mioche et al., 2015). These clouds are generally composed of one or several distinct stratiform layers consisting of supercooled water droplets embedded near the top of an ice cloud (Curry et al., 2000;Korolev et al., 2003;Shupe et al., 2011). Single-layer stratocumulus MPCs have been extensively studied in the western and European Arctic (Shupe et al., 2006;Gayet et al., 2009;McFarquhar et al., 2011;Morrison et al., 2012;Lloyd et al., 2015;Mioche et al., 2017;Achtert et al., 2020;Järvinen et al., 2023). ...

FIRE Arctic clouds experiment

Bulletin of the American Meteorological Society

... The National Research Council of Canada's Convair-580 research aircraft is a twinengine pressurized aircraft that was modified to conduct investigations of atmospheric phenomena and is capable of carrying up to a dozen scientists. The aircraft has an extensive history of collecting data for aircraft icing studies (Cober et al. 1995;Isaac et al. 1999Isaac et al. , 2001Isaac et al. , 2005Williams et al. 2015;Minder et al. 2023). The Convair-580 carried an array of navigational, cloud physics, and atmospheric chemistry instrumentation during the ICICLE campaign. ...

Recent Canadian Research on Aircraft In-Flight Icing.

... 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. ...

Aeromagnetic Gradiometry Methods - A Study Using Real Data.
  • Citing Article
  • 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. ...

Preliminary Analysis of Data from the Lincoln Sea Aeromagnetic Surveys 1989-90.
  • Citing Article
  • January 2010

... There are several studies presenting approaches to explain the development of precipitating freezing drizzle. The interested reader is referred for example to Cober et al. (1996) or Korolev and Isaac (2000). Even if the super-cooled drops are not large enough to precipitate, they may pose a significant threat for aircraft crossing the cloud, as they freeze on contact as well. ...

Analysis of Aircraft Icing Environments Associated with Supercooled Drizzle Droplets.

... 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]. ...

Comments on “Magnetic Field Gradients and Their Uses in the Study of the Earth's Magnetic Field” by Harrison and Southam
  • Citing Article
  • January 1992

Journal of geomagnetism and geoelectricity

... (3). To determine C β , yawing maneuvers were used, which are commonly applied for such calibration (e.g., Bögel and Baumann, 1991;Drüe and Heinemann, 2013;Mallaun et al., 2015;Williams and Marcotte, 2000). In a first step, the wind vector is calculated for a yawing maneuver. ...

Wind Measurements on a Maneuvering Twin-Engine Turboprop Aircraft Accounting for Flow Distortion
  • Citing Article
  • June 2000

Journal of Atmospheric and Oceanic Technology

... There are many applications where FSSP is used especially when droplet spectra are required. Cober et al. (1995Cober et al. ( , 1999, based on works of Ashenden and Marwitz (1998) and Miller et al. (1998), give the case of aircraft icing characterizations, as an example of FSSP use. Cober and Isaac (2012) highlighted the interest of FSSP for the measurements of the super large droplet characterisation. ...

Measurements of Aircraft Icing Environments Which Include Supercooled Large Drops.