Aerosols Nearly 1000 Miles Long & EM-Charged Prairie Storms

Aerosols seen stretching across north-west WA and Okanagan BC,
pointing NE towards Edmonton, AB

Prior to an intense Edmonton storm (July 10), our team of Skywatchers have discovered an aerosol plume stretching nearly a thousand miles, across the Pacific and British Columbia. We believe that this was a heavy aerosol-spraying operation. The developing aerosols can be seen here. Closer detail of the aerosol movement can be seen with Intellicast here. A sky time lapse of this aerosol system going over Washington can be seen here and here. What is interesting about this aerosol system is its enormous length and the timing of Doppler / NEXRAD stations becoming very active during this time, further driving in the moisture-collected aerosol clouds to desired areas. Furthermore, these aerosols appear to be related to a weather system that developed near Edmonton and other nearby areas during that time. Take note of how a storm develops at the tip of this aerosol plume extending into Alberta near Edmonton.

During the time which these aerosols were moving across parts of Washington and Oregon, we see very active NEXRAD-pulsing and electromagnetic (EM) activity in Portland, OR, and especially Seattle, WA NEXRAD stations. Interestingly Langley Hill, WA NEXRAD station had its data conveniently missing during this time. 

Approximate orientation of the aerosol plume, lining up with 
active NEXRAD stations (the yellow pins)

These aerosols that stretched across British Columbia conveniently line up with active NEXRAD / Doppler stations, pointing directly towards the Doppler station in Edmonton, AB. In Naramata, BC, we can see the aerosols appearing in the sky (above the cumulus clouds), and the clouds seem to be moving along the same orientation as the plume, while the aerosols actively collect moisture. We believe the aerosols not only to be influenced by NEXRAD / Doppler EM activity, but also gaining help from the wind pattern for July 10.

Aerosol plume collecting moisture, passing through the Pacific region,
towards the Kelowna Doppler region, and directed
towards Edmonton, AB

In watching where the moisture appears to be travelling, the Doppler stations for the Pacific region can be viewed here. Interestingly, Victoria's Doppler station has missing data during this time in which we see the Prairie Doppler stations (and Edmonton) pulsing intensely. Noting that the data is conveniently missing for the Victoria station (and Langley Hill, WA), during the time which the aerosol plume forms near Victoria, it makes us wonder if moisture is actively being fed from the coast. We see moisture / clouds being fed into Edmonton, AB through the Grand Prairie Doppler station (mostly) and the Kelowna Doppler station. Edmonton Doppler animation can be viewed here. The cloud system coming from Grand Prairie appears to have originated from the Prince George Doppler station that attracted moisture from the east. The cloud system arriving into Edmonton from the Kelowna Doppler station can be viewed here. In that video, we can clearly see moisture / clouds being driven north east directly towards Edmonton, AB. 

Edmonton, AB: The high altitude aerosols seen on July 10th seems to be
filled with electromagnetic signature prior to the storm

We can see the Edmonton Doppler station appears to be very active during the time which the storm rolls in from the north west, and clouds coming in from the south west. Furthermore, we see the storm heads directly east, and a linear feature can be seen driven south-east. The storm system appears to have been influenced by the Edmonton Doppler station. 

The most recent Prairie radar data can be seen here, and during this time (July 10, 22:00 MDT) we see Saskatoon and Regina Doppler stations pulsing intensely, which can also be seen here (July 11, 04:00 MDT). The National Radar for these events can be seen here. After taking a
closer look at the Saskatoon Doppler station, we initially see a quiet radar, and afterwards we see intense electromagnetic activity pick up, which appears to be charging a storm system south east of the Doppler centre. This occurs again later in a similar fashion. The cloud system south east of the radar centre appears to be actively affected by EM waves emitted from the Doppler station. This type of storm generation can also be seen near the Regina Doppler station, which also appears to be super-charging a storm in the south east quadrant during the same time. Afterwards, we see strong EM activity north east of the Doppler station, later sending out energy to the south-west and north-west, while continuing to send out energy towards the north-east. 

On the left image, we see moisture lined up to the south east of the radar centre. On the right image, we were able to portray these EM lines going out from the centre of the radar through the linear portions of the storm. Could electromagnetic waves emitted from the centre of the Doppler station explain this strange phenomenon we are seeing?

We must ask ourselves what is causing these mysterious storms to appear around the circumference of the Doppler stations? We also note the wind patterns for Saskatchewan during this time (July 11) is north. Furthermore, we must also take into consideration the weather system moving north-east, originating from the States into Montana and the lower Prairies. Keeping in mind that the wind is moving north, what is causing these storms on the radar to have this lineation oriented towards the centre of the radar if it is not electromagnetically-induced weather?

Edmonton, AB: The wicked storm that was shown advancing on the Doppler radar. The linear features of
EM cloud influence seem to correlate well with what we saw on the Doppler radar.

Edmonton, AB: Rotating clouds seen by one resident on July 10th

Edmonton, AB: Storm photographed by a resident and photo-enhanced ,
showing the strange EM-induced shape

One resident showing the size of hail dropped in some areas of Edmonton, AB

Edmonton, AB: Photograph of strange-shaped hail, appearing to be somewhat flattened

Ootischenia, BC: A last glimpse of the aerosols seen passing through the
Kootenay Valley on their way towards Alberta on July 11. Paused at this satellite image, note the fork of
aerosols -- one  path seen going through the Kootenay Valley, and another path going through the Okanagan Valley.

Windfield, BC: Aerosols seen passing through the Okanagan Valley on July 11th on their way to Alberta

Above: Photos taken by a local resident near Portland, OR, showing these aerosols stretching across the sky on July 11, at 6:45 am (PDT). In the first photo, the left shot is looking towards Mt. Hood (south), and the right shot is facing West. In the second photo, the top shot is again looking towards Mt. Hood (south) and the bottom shot is looking up the Hood River Valley.

Alberta being fed more Rain from NEXRAD-induced Weather

Many areas in southern Alberta are still recovering from the intense flooding that took place in late June, displacing many thousands of residents. There have been numerous other EM-induced storms in July that have been causing flash flooding and intense hail damage in many areas. We will present information as to the recent rain and cloud system we received in southern Alberta on July 7th and 8th. There has been no mention in the weather media of the tapering aerosol cloud plumes originating in the North-western States, which brought majority of the rain to southern Alberta. We will present evidence as to how these cloud systems have been generated precisely near the NEXRAD / Doppler stations using electromagnetic waves, and thereafter pushed into southern Alberta, bringing more rain to the flood-ravaged area. The NEXRAD stations which are of interest to us with regards to originating the cloud plumes are located near Portland, OR; Spokane, WA; and Boise, ID. A playlist for the events and weather data of July 7th can be seen here, and a playlist for July8th can be viewed here.

NEXRAD-induced cloud systems: We can clearly see three significant cloud plumes originating from NEXRAD stations in the U.S. The first plume (red) is from the NEXRAD station in Portland, OR. The last plumes (red and magenta) are originating from the NEXRAD stations in Spokane, WA and Boise, ID, respectively. We also noted a small plume originating from what appears to be a NEXRAD station in Medford, OR, and from the video, it appears to be pushed towards the Boise, ID station.

After watching the above satellite animation for July 7th - 8th, we can clearly see a tapered cloud plume originating near Portland, OR and later feeding into southern Alberta. A one hour loop from Intellicast satellite animation shows this plume in more detail. What is interesting about this plume is that it appears to be heavy aerosol sprayed off the West coast of Washington / Oregon, if not mistaken for the similar-looking cirrus clouds . However, after watching sky time lapse videos for areas near the coast, we can see that these appear to be aerosols advancing through the sky here and here. In Happy Valley, OR, this video was also captured, which shows the moisture-collected aerosols that have the signature of strong electromagnetic pulsation, causing the linear shape of this metallic-laced aerosol plume. This was also confirmed by residents living in these areas, as well as video footage here and here.

NEXRAD Station (KRTX) for Portland, OR

The NEXRAD animation data for Portland, OR during the time which this aerosol plume was influenced can be viewed here. After watching this video, we can clearly see the NEXRAD station initially with very quiet activity, and then suddenly pulsing at this time, which we believe may be the electromagnetic attraction of the aerosol plume. The station then shortly ceases this EM-pulsing in all directions, and sends out what appears to be an electromagnetically-charged beam in the north east direction. Immediately thereafter, we can see the plume begin to originate just as was seen on the satellite animation, oriented in the same north east direction.

We can see that the plume driven from the Portland NEXRAD station is not only moving east, according to the natural wind flow pattern, but it is also moving north , which is not consistent with the wind patterns at that time. After viewing the animated data for wind movement in this area, we must ask ourselves what is driving this plume north if it is not electromagnetic forces emitted precisely from these NEXRAD stations? Although we believe that NEXRAD works alongside with wind, there are some experts suggesting that our wind patterns are being changed due to heavy Geoengineering operations. However, in this situation we see natural winds moving slightly east and south, not north.

July 7th: Calgary skies prior to the storm system arriving the next day

The Alberta skies time lapse during July 7th can be viewed for Calgary, AB here, and for Didsbury, AB here. Pictures for July 7th of Calgary skies can be viewed here. What appeared to be high altitude clouds (or aerosols) oriented south East-West advanced into Calgary prior to the storm system arriving the following day. An electromagnetic signature can be seen in the photo pictured left, showing the NEXRAD / Doppler effect in some of these high altitude clouds. This cloud system appears to be linked to north-west Montana, and some sky time lapse videos for Montana (NW) can be viewed here and here. The clouds in those areas of Montana's sky also appeared to be slightly pulsed.

Plumes created from NEXRAD stations near Spokane, WA
and Boise, ID, bringing more rain into southern Alberta

Later throughout the satellite animation, we see two more plumes created at NEXRAD stations near Spokane, WA and Boise, ID on July 8th. Cloud plume generation for the Spokane NEXRAD station can be viewed here, and the NEXRAD data for Boise, ID can be viewed here. During this time was when southern Alberta received most of its rain for this day. A time lapse video for Calgary, AB shows the heavily-pulsed aerosol cloud system arriving from Washington and Idaho state prior to the rainfall. Doppler radar animation for July 8th in Calgary, AB can be viewed here. We believe this storm system was further pushed north-east into southern Alberta with the help of nearby Doppler stations in Canada. Additionally, we have noted an intense electromagnetic blast at 5:20 and 6:20 pm (MDT) from the Doppler station located near Vernon, BC, which we believe caused the north-east advancing storm to be pushed further east. We also find it interesting that in the morning of July 8th, we see a small storm system initially just West of High River, AB later being pushed directly through the centre of the Strathmore Doppler station here.

We will add more material as it comes along from other residents in the area. If you have any information, photos, or videos, please email: weatherpeace@gmail.com

Calgary, AB: July 8th - Electromagnetic pulsing seen throughout the NEXRAD-blanketed skies

Calgary, AB: Evening of July 8th - After the receding storm, NEXRAD leaves its linear plume marks in the sky

Calgary, AB: The evening sky displaying its electromagnetic signature throughout the clouds 

Calgary, AB: The sky facing north, showing this NEXRAD-induced linear front in the clouds