Sentence examples for storm variations from inspiring English sources

Exact(3)

First, note that the source of geomagnetic storm variations is assumed to be large-scale (at least at non-polar latitudes), and therefore external coefficients of relatively low n and m (≤ 3) are used to describe its spatial structure.

The modeling technique is based on the empirical formulation of the ionospheric storm variations in respect to interplanetary magnetic field (IMF) disturbances, on the determination of the type and the amplitude of the ionospheric response in each local time sector as well as on the estimation of the time delay of the ionospheric disturbance onset in respect to the storm onset disturbances.

Using the observed geomagnetic storm variations to construct a geomagnetic profile to stimulate the rats, we found that the geomagnetic field variations associated to the SSC day were capable of increasing the subjects AP between 7% and 9% from the reference value.

Similar(57)

Further improvements in accuracy may occur once decadal wave hindcasts include storm surge variations in water levels, and have increased nearshore resolution.

The dashed lines in the upper panels show the storm time variations of internal part B i and external part B e out of the disturbed horizontal field B θ of dipole symmetry; B θ fields appear as solid lines.

It bears mention that Pachyderm is not the only open source platform currently aiming to provide an alternative to Hadoop MapReduce when it comes to processing large amounts of data: Apache Spark and Storm are variations on a similar theme, and languages such as Scala have emerged to make using Hadoop easier.

Rastogi (2006) shows that storm time variations of the H-range are largest at stations close to the magnetic equator and at the midday longitudes from data at stations in India between −0.7° and 45.2° in magnetic latitude for the 17 18 November 1989 and the 20 21 February 1992 events.

Alternating beach ridges and swales represent events of storm intensity variation during falling late Holocene SL.

In ERG team, Nagoya University has developed the radial diffusion model and simulated the storm-time variations as well as the solar cycle variations (Miyoshi et al. 2003, 2004).

We show two examples of observed GICs at the Memanbetsu substation associated with the geomagnetic storms with variations of geomagnetic fields at the Memanbetsu Observatory.

During this period of the geomagnetic storm, the variation in GPS-TEC was from 10 to 50 vertical TECU at the given point.

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