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Date/Time: 12/04/2013 10:15:09 UTC
Lat: 86.9867 Long: 57.2069
Magnitude: 4.4M/4.6 mb
Depth: 2 km
Location: NORTH OF FRANZ JOSEF LAND
Catalog Source: emsc, gfz and usgs
TTNT energy released: 119.7866
Date/Time: 12/04/2013 10:27:46 UTC
Lat: 86.02 Long: 67.83
Magnitude: 2.45 ML
No. of Stations:
Depth: 13.8 km
Location: NORTH OF FRANZ JOSEF LAND
Catalog Source: NORSAR
ID:
TTNT energy released: 0.0714
There was a lot more grey in that area early this morning.
The most widely used instrument for ionospheric measurement is the ionosonde. The ionosonde is essentially a high frequency radar which sends short pulses of radio energy into the ionosphere. If the radio frequency is not too high, the pulses are reflected back to earth.
The ionosonde records the time delay between transmission and reception of the pulses. By varying the frequency of the pulses (typically 1-22MHz), a record is obtained of the time delay at different frequencies. This record is referred to as an ionogram.
Originally posted by PuterMan
reply to post by radpetey
There was a lot more grey in that area early this morning.
Just to remind you that the area of TEC disturbance basically follows the area of maximum insolation and therefore rotates around the world in a 24 hour period.
Believe me I have downloaded the NASA/JPL TEC maps every 5 minutes 24/7 for over a year (I have stopped now with over 150,000 images under my belt cluttering up disk) and I can find absolutely no correlation at all between the maps and the incidence of earthquakes.
These maps are actually theoretical being the predicted TEC affecting communications and are just simply NOT sophisticated enough to detail what the scientists look at for TEC changes before an earthquake.
The details on these maps are actually taken from ground based GPS stations - you can find lots of details on how it works - however the ones the scientists use are satellite based. Not the same thing at all. (See the post above this about the Demeter satellite)
Don't mean to burst anyone's bubble but in my honest opinion these particular TEC maps are of no use to us in pre-determining earthquakes.
I still put a version of the TEC map in with my earthquake reports, but it is probably a waste of time.
edit on 14/4/2013 by PuterMan because: (no reason given)
ETA:
The most widely used instrument for ionospheric measurement is the ionosonde. The ionosonde is essentially a high frequency radar which sends short pulses of radio energy into the ionosphere. If the radio frequency is not too high, the pulses are reflected back to earth.
The ionosonde records the time delay between transmission and reception of the pulses. By varying the frequency of the pulses (typically 1-22MHz), a record is obtained of the time delay at different frequencies. This record is referred to as an ionogram.
I note that the Australian site refers to HF radar so maybe my comment that they use GPS stations is out of date? Don't really know and haven't the time to find out.
Basically what is does show is that these maps are based on GROUND BASED systems and not the same sa the satellites at all.
edit on 14/4/2013 by PuterMan because: (no reason given)
Did the slide show up on the mine lists?
4.2 ; M
8km ENE of Luther, Oklahoma ; Location
2013-04-16 10:16:53: Time
35.687°N : Lat.
97.109°W : Lon.
5.0: D
3.3: M
7km E of Luther, Oklahoma: Location
2013-04-16 07:16:43 Time
35.650°N: Lat
97.117°W : Lon.
5.0: D
2.8: m
14km NNW of Boley, Oklahoma: Location
2013-04-16 07:15:36: Time
35.608°N: Lat
96.558°W: Lon
5.0: D
4.3: M
12km ENE of Luther, Oklahoma: Location
2013-04-16 06:56:30: Time
35.685°N: Lat
97.066°W: Lon
5.0: D
3.0: M
5km WSW of Chandler, Oklahoma: Location
2013-04-16 06:45:27: Time
35.677°N: Lat
96.940°W: Lon
4.9: D
3.0: M
18km SE of Old Faithful Geyser, Wyoming: Location
2013-04-16 09:46:48: Time
44.329°N: Lat
110.686°W: lon
8.3: D
7.8: M
86km ESE of Khash, Iran: Location
2013-04-16 10:44:13: Time
28.056°N: Lat
62.080°E: Lon
15.2: D