The patent badge is an abbreviated version of the USPTO patent document. The patent badge does contain a link to the full patent document.

The patent badge is an abbreviated version of the USPTO patent document. The patent badge covers the following: Patent number, Date patent was issued, Date patent was filed, Title of the patent, Applicant, Inventor, Assignee, Attorney firm, Primary examiner, Assistant examiner, CPCs, and Abstract. The patent badge does contain a link to the full patent document (in Adobe Acrobat format, aka pdf). To download or print any patent click here.

Date of Patent:
Apr. 07, 2020

Filed:

May. 05, 2017
Applicant:

Rosemount Aerospace Inc., Burnsville, MN (US);

Inventors:

Vincent R. LoPresto, Eagan, MN (US);

Mark Sherwood Miller, Lakeville, MN (US);

Assignee:

Rosemount Aerospace Inc., Burnsville, MN (US);

Attorney:
Primary Examiner:
Assistant Examiner:
Int. Cl.
CPC ...
B64D 15/22 (2006.01); B64D 15/20 (2006.01); B64D 47/02 (2006.01); B64D 47/08 (2006.01); G01N 21/55 (2014.01); B64C 1/14 (2006.01); H04N 7/18 (2006.01);
U.S. Cl.
CPC ...
B64D 15/22 (2013.01); B64C 1/1484 (2013.01); B64D 15/20 (2013.01); B64D 47/02 (2013.01); B64D 47/08 (2013.01); G01N 21/55 (2013.01); H04N 7/183 (2013.01);
Abstract

Apparatus and associated methods relate to projecting a light beam onto an interior surface of an aircraft window so as to indicate a testing location to test for ice accretion. The testing location is determined, by a boundary locator, based on aircraft flight conditions, aircraft exterior shape, and a predetermined size of super-cooled droplets, which could present a hazard to the aircraft. The determined test location corresponds to a calculated boundary that separates locations where super-cooled water droplets of the predetermined size cause ice-accretion from locations where such particles do not cause ice accretion, for such aircraft flight conditions. The light beam is then projected onto the interior surface of the aircraft window at the determined test location. The projected beam of light can indicate, to an observer and/or a detector, a location to monitor for ice accretion caused by super-cooled water droplets of the predetermined size.


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