Calgary, AB, Nov 26-27/13 - With its linear shape, many are calling it a Chinook. However, we must keep in mind the mass of linear aerosols that were being sprayed prior to this formation, along with the diminished EM (electromagnetic) emissions in the Rocky mountainous regions. There are next to no cellphone towers or Doppler facilities at those rocky heights. This mass of linear "clouds" were originally sprayed aerosols that collected moisture and were further pulsed into shape by EMF (electromagnetic frequency). The linear cloud formation was kept in place by EM frequency, hovering over Calgary for over 13 hours, as it later shifted towards Montana's Missoula and Great Falls NEXRAD regions to be also held in place for 13+ hours, with the same linear edge. Many locals are calling this a Chinook, but is there more to it? The full playlist of events can be seen here.
Nov 26/13, 15:07 UTC - EM blast emitted from Great Falls, MT NEXRAD Station. Shortly after this, we see the linear cloud front move into this region (on the satellite video).
Oct 9/13 - The climate engineers have been at useless work the past few days. Sprayed aerosols were spotted in Calgary, AB. Towards the evening, the linear mat of collected aerosols can clearly be seen towards the West, oriented SW-NE. They can also be seen on satellite images, sucking up moisture, specifically going through NEXRAD-active regions. The NEXRAD sites are shown as dots in the two last images, and moisture can be seen channelling through these areas.
Sept 24/13 - Climate Engineering in a nutshell: Spray metallic aerosols inland and over ocean while a tropospheric river is advancing towards land. These metallic particles rob water vapour from the air to form "clouds", thus diminishing cumulus clouds' ability to form. With the NEXRAD / Doppler network working in unison, an enormous "cloud front" can be created. These metallic-laced clouds can be shaped and directed with electromagnetic wave frequency i.e. using NEXRAD radar stations, like the one shown centred in the 4th frame of the image below:
The first photos were taken in Calgary, AB in the morning, showing how the sky later became a white mass of "cloud" cover. The photos that follow respectively are: satellite images of cloud cover, photos taken from Washington and Oregon, and radar images showing NEXRAD influence on this approaching weather front coming from the San Francisco, Sacramento, and Eureka, CA Doppler stations. Reno, Nevada NEXRAD station also shows electromagnetic influence on the weather front as can be seen with the linear feature going directly through the centre of the radar circumference.
Today, Calgary residents witnessed a morning sky whose incoming clouds were filled with Doppler ripples and signs of electromagnetic signature. A time lapse of our sky can be viewed here. A map of all sky time lapse videos can be viewed here, in which Washington and Oregon state can be accessed on the right side of that page.
We have tracked this cloud system originating precisely from NEXRAD stations in Washington and Oregon, and have documented its movement using radar and satellite animation. The full playlist of all events can be seen here. In the satellite animation, pay close attention to where the tapering plume-shaped clouds originate from in Oregon and Washington, only to be later pushed into Alberta using Canadian Doppler Stations.
Above: Photos depicting Calgary's sky on July 17, roughly 11:00 am, facing East. Notice the linear arms of this storm system that are similar to the pulsing anomalies we see in radar viewed from Doppler stations. We believe that the Doppler stations are helping to move these clouds, and as a result shapes them with electromagnetic signatures.
We can clearly see clouds being generated as plumes in Oregon and Washington NEXRAD Stations, which are then driven north east into British Columbia, with the help of Canada's Doppler stations co-operating to bring this cloud system into Alberta. Most of the moisture and clouds are being driven north east from the Spokane, WA Station towards the Vernon Doppler station to end up in Alberta and eventually Calgary.
Above: The left image shows specific NEXRAD Stations in the U.S. that are of particular interest to us, because they are involved in generating the strange plume-shaped clouds that are pushed north into Canada. The right image shows the Canadian Doppler stations working in conjunction to further drive this moisture north into British Columbia and eventually Alberta.
Above: Satellite image of Western Canada on July 16, 19:30 UTC. Pay attention to the tapering plume
generated near Medford, OR on the bottom left.
Above: Medford, OR NEXRAD Radar: Tapering plume generated precisely from the Medford, OR (KMAX) Station
Above: Western Canada satellite image for July 17, 5:00 UTC. Pay close attention to the plume-shaped clouds generated at Portland, OR (left) and Pendleton, OR (right).
Above: Portland, OR (KRTX) NEXRAD Station on July 17, 5:02 UTC, generating a tapered
cloud system that was seen on satellite images.
Above: Pendleton, OR (KPDT) NEXRAD Station on July 17, 5:03 UTC, seen generating a tapering
plume-shaped cloud system as seen on satellite images.
Above: Western Canada satellite image for July 17, 17:30 UTC. Pay attention to the plume-shaped cloud
system originating near Spokane, WA.
Above: Spokane, WA (KOTX) NEXRAD Station on July 17, 17:44 UTC, seen
generating a tapered plume-shaped cloud system.
Above: Vernon, BC (Silver Star Mountain) Doppler Station receiving the cloud system that originated in Washington, and driving this system towards the Calgary Doppler Station. The time is July 17, 16:30 UTC.
Above: Strathmore, AB (near Calgary) Doppler station receiving the cloud system from British Columbia (Vernon Doppler Station), that originated from Washington. The timing is July 17, 16:30 UTC (10:30 a.m. MDT).
Above: Calgary's sky, facing north. We see the electromagnetic ripples as signs that a Doppler station has left its mark on these clouds. This is the signature of electromagnetic-induced clouds. All morning photos can be viewed here.
Here is the weather satellite animation data for Western Canada, regarding the storms developing in southern Alberta. The playback is July 3 - 6.00 am to July 4 - 11.00 pm MST. Take note of where the strange tapering plumes (storms) are developing in S.Alberta. We are uncertain of where the source of this cloud formation is being fed from.
On July 4th, Calgary residents and others in southern Alberta were issued a tornado warning from Environment Canada. What was not mentioned to the public was the censoring of our weather data.
During this animation playback above, take note of the screen blackout which occurs on July 3 immediately after 20:30 UTC. We are astonished at the amount of data that was taken out of this loop. There is a large segment missing between July 3, 20:30 and July 4, 6:00 UTC. These frames have been removed from the satellite images. We believe this data has been intentionally censored out, prior to the developing severe storm in southern Alberta. Several Doppler stations in Western Canada also had their data removed during this time, prior to heavy electromagnetic pulsing coming from the NEXRAD / Doppler stations in the Prairies region. We also checked the data for Eastern Canada, and noted similarly this censoring to the public in selected areas. Furthermore, we also noted that July 4, 19:30 - 20:30 UTC (1:30 - 2:30 pm MST) has been censored out.
Several Doppler stations in Western Canada have had their data censored from the public. Prior to almost all stations appearing blank, note the strong EM-pulsation at the Prairie stations, such as Calgary, Medicine Hat and others.
We have provided several Doppler animations for review of the developing storms in southern Alberta here. From the detailed video, we can see that the storm initially begins near Wetaskiwin, AB, in which we are uncertain of where exactly all this moisture is coming from. The Doppler station (centred at Strathmore, AB) becomes very active in what appears to be generation of plasma clouds shortly afterwards, driving the growing storm system south. This can be seen better by looking at the plasma clouds generated around the Doppler station that have become concentrated, pointing towards the storm system. During this time, the sky in parts of Calgary went from blue to a thin blanket of white. This can be further analysed in our weather time lapse video. In that video, pay close attention to the artificial ionospheric plasma clouds produced by nearby Doppler stations that can generate electromagnetic waves in the same frequency range as HAARP. These EM-induced clouds can be seen driven by EM frequency (from Doppler station) from right to left in the video. Then shortly afterwards, we see the developing storm system is driven in from left to right, advancing in the opposite direction.
At this point, it becomes more clear to see the straight-edged cloud system that has formed, using EM frequencies emitted from the Doppler station. This is further manifested when one takes a close look at the thin and bent linear arm that is pulsed in the same direction. During this time, further strange anomalies can be seen near Lake Louis, which is pictured below:
Doppler station at Strathmore, AB: Note the strange linear arm (at centre) being driven south along with the storm system, towards the Doppler centre using electromagnetic frequencies. Another strange anomaly can be seen near Lake Louis (left), as three bent linear arms of clouds have become stretched, mimicking the circumference of the radar.
Once the west arm of the storm system has reached the centre of the Doppler station, and after EM pulsation from the Doppler station has appeared to cease, the storm system stops going south and resumes its natural motion east. Meanwhile, there are other numerous storm systems developing south of Calgary, during the video playback.
Video footage of the storm making its way into northern Calgary (6:30 pm) can be seen here. Note how the southern end of the storm is well defined by its linear (radar-pulsed) edge. This also seems to be consistent with the radar at this time. The storm system appeared to be moving very fast, despite the apparent wind speed. Very low clouds were also spotted separately moving below this system.
We noted that the cloud system near the Rockies seems to appear quiet in the beginning of the video, however, as soon as the Doppler station becomes active in pulsing, one can see stretched cloud
systems being driven north east directly towards the Doppler station centre. Furthermore, note the strange cloud system forming near Hanna, AB here. It appears to hold very little moisture, and has no apparent source for its cloud development.
There may be more strange anomalies and other natural formations not discussed in the length of this entry. Please notify us if you come across anything interesting.
Red Deer, AB: This is a photograph sent in by one of our Skywatchers, facing north as the storm system passed over this town. It is interesting to note the shape of these clouds, which are referred to by meteorologists as mammatus clouds. However, one must consider how these clouds form in response to artificial radiative heating from EM waves emitted by ground or air-based devices.
Calgary, AB: NEXRAD-pulsed clouds prior to the storm
Calgary, AB: On-lookers stand in astonishment, viewing the intensity of this strange storm
North-east in Calgary, AB: In this photograph, an unusually low, long tapering cloud appears to be moving from left to right, immediately above the houses
Could this be the linear bent arm we saw being driven south in the radar?
Another photograph showing the intensity of this oncoming storm
The first photos were taken in Calgary, AB in the morning, showing how the sky later became a white mass of "cloud" cover. The photos that follow respectively are: satellite images of cloud cover, photos taken from Washington and Oregon, and radar images showing NEXRAD influence on this approaching weather front coming from the San Francisco, Sacramento, and Eureka, CA Doppler stations. Reno, Nevada NEXRAD station also shows electromagnetic influence on the weather front as can be seen with the linear feature going directly through the centre of the radar circumference.
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