Sentence examples for these declination from inspiring English sources

The songbirds migrating across the North American continent may therefore have adapted to a system of re-calibration of compass information to cope with these declination variations met during migrations (Able and Able, 1990a; Able and Able, 1993; Able and Able, 1995).

These are the declination (the angle between the line axis or torus normal and the z axis of orthogonal coordinate system used in CRYSTALS) and the azimuth (the angle between the projection of the line axis or torus normal onto the x-y plane and the x axis of the orthogonal coordinate).

In the equatorial coordinate system, the right ascension coordinates of these borders lie between and, while the declination coordinates are between −60.26° and −70.51°.

In the equatorial coordinate system, the right ascension coordinates of these borders lie between and, while the declination coordinates are between and.

In the equatorial coordinate system, the right ascension coordinates of these borders lie between and, and the declination coordinates are between −55.43° and −70.62°.

In the equatorial coordinate system, the right ascension coordinates of these borders lie between and, while the declination coordinates are between 31.10° and −1.35°.

The official constellation boundaries, as set by Eugène Delporte in 1930, are defined by a quadrilateral; in the equatorial coordinate system, the right ascension coordinates of these borders lie between and, while the declination coordinates are between −11.03° and −33.25°.

These included patient declination of evaluation (16 cases), frequent patient-initiated appointment cancellations (4 cases) and no-shows (9 cases), comorbid medical conditions (16 cases), comorbid psychiatric diagnoses (8 cases), and homelessness (1 case).

These remanence directions are shown in a specimen coordinate frame; therefore, the declination values are directly influenced by the accuracy of orienting the marker lines with a laser level, but the inclination values are determined only by the ratio of the in-plane and axial components measured with a single fluxgate sensor.

The polar axis supports the declination axis of the instrument.

Several hypotheses have been proposed to explain these variations, they can be solar wind driven and/or induced by the geometrical effect of the declination of the Earth in the jovicentric coordinates, DE.