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The anomaly times were provided in SND only for Aqua (1500 UTC), Midori (2349 UTC), HST (1234 UTC), and ICESat (0258 UTC).
SND provides only a limited number of anomaly times and is given mostly in Coordinated Universal Time (UTC); therefore, it is important to determine the SLT because of its relationship with the migration of energetic particles owing to magnetic perturbations.
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Along-track empirical tidal constants derived from X-TRACK Sea Level Anomaly time series are also used to validate tidal models.
It is tailored for extending the use of altimetry data to coastal ocean applications and provides freely available along-track Sea Level Anomaly time series that cover today all the coastal oceans.
By using estimates of the ages of oceanic crust obtained from core samples by deep-sea drilling, a magnetic anomaly time scale was constructed, and at the same time the spreading history for the ocean basins covering the last 200 million years or so was proposed.
Failure descriptions, along with the anomaly time, were used to construct the criteria to select the LEO satellites for analysis.
We created an anomaly time series for each of these quantities and then normalized them by their SD (anomaly and SD with respect to 2000 2013 June-July average, SD based on all days in each time series) giving SDs of 2.5°C, 2.1°C, and 2.9°C for IST, T2m, and T500, respectively.
The daily MODIS melt anomalies were derived, and the MODIS melt index was formed, by normalizing the anomaly time series by its SD: We selected Z500 and T500 fields from the days when the melt index exceeded 1 SD (in absolute terms).
The anomaly time series for each month are plotted in Fig. 6c.
(c) NIÑO4 sea-surface temperature anomaly time series (http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ensoyears.shtml).shtml
The start of the year is anomaly time and the ladder looks bizarre next to pre-season predictions.
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