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Fred Remer
เข้าร่วมเมื่อ 5 เม.ย. 2015
This channel is a collection of narrated PowerPoint presentations and other videos of theoretical meteorology and aviation. I am an associate professor at the University of North Dakota in the Atmospheric Sciences department.
วีดีโอ
ATSC 210 Lab1 Surface Obs - Special Criteria
มุมมอง 20911 หลายเดือนก่อน
ATSC 210 Lab1 Surface Obs - Special Criteria
ATSC 231 Thunderstorm Avoidance - Preflight
มุมมอง 258ปีที่แล้ว
ATSC 231 Thunderstorm Avoidance - Preflight
ATSC 231 Convective Wind Shear - Detection & Alerts
มุมมอง 175ปีที่แล้ว
ATSC 231 Convective Wind Shear - Detection & Alerts
ATSC 231 Convective Wind Shear - Model Actions
มุมมอง 179ปีที่แล้ว
ATSC 231 Convective Wind Shear - Model Actions
ATSC 231 Convective Wind Shear - Inadvertent Encounters
มุมมอง 219ปีที่แล้ว
ATSC 231 Convective Wind Shear - Inadvertent Encounters
ATSC 231 Convective Wind Shear - Weather Producers
มุมมอง 191ปีที่แล้ว
ATSC 231 Convective Wind Shear - Weather Producers
ATSC 231 Thunderstorm Hazards - Turbulence
มุมมอง 236ปีที่แล้ว
ATSC 231 Thunderstorm Hazards - Turbulence
ATSC 231 Intro to Thunderstorms - Climatology
มุมมอง 245ปีที่แล้ว
ATSC 231 Intro to Thunderstorms - Climatology
ATSC 231 Non-Convective Low Level Wind Shear 4
มุมมอง 166ปีที่แล้ว
ATSC 231 Non-Convective Low Level Wind Shear 4
ATSC 231 Non-Convective Low Level Wind Shear 3
มุมมอง 280ปีที่แล้ว
ATSC 231 Non-Convective Low Level Wind Shear 3
ATSC 231 Non-Convective Low Level Wind Shear 2
มุมมอง 279ปีที่แล้ว
ATSC 231 Non-Convective Low Level Wind Shear 2
ATSC 231 Non-Convective Low Level Wind Shear 1
มุมมอง 360ปีที่แล้ว
ATSC 231 Non-Convective Low Level Wind Shear 1
ATSC 231 IFR Conditions 2 - Other Obscuring Phenomena
มุมมอง 148ปีที่แล้ว
ATSC 231 IFR Conditions 2 - Other Obscuring Phenomena
ATSC 231 IFR Conditions 1 - Low Ceilings 1
มุมมอง 204ปีที่แล้ว
ATSC 231 IFR Conditions 1 - Low Ceilings 1
Please upload more of these!! They’re great
.
1993 the year y'all started f with the p around them just saying
Hu that is interesting
In 1974 I had the great experience of flying hail suppression (base seeding and top seeding) in a combined suppression/research project (Alberta Hailstop '74). In 'those days' our understanding of the detailed airflow around these storms was less clear. While I and my colleagues were flying cloud seeding missions, the scientists/meteorologists on the project were flying updraft penetrations in Cessna 414 equipped with cloud physics sensors. I learned a lot about SAFELY maneuvering around thunderstorms and this knowledge proved to be a great advantage for my airline career that followed. Your analysis and radar images here are a great training aid for any pilot. This understanding, along with our industry standard recommendations for circumnavigating this kind of weather, serves us well. My main 'beef' is that airliner radars only pitch upwards to 15 degrees and become somewhat useless for terminal area (close in) weather avoidance. Then we become much more dependant upon ATC 'suggestions,' PIREPS, and our own visual analysis out the front windows. Thanks for sharing this slide show.
very helpful video
Great video, very helpful!!
Thank you sir 😊
In the 1990s, the 'second generation' mobile phone systems emerged. Two systems competed for supremacy in the global market: the European developed GSM standard and the U.S. developed CDMA standard. These differed from the previous generation by using digital instead of analog transmission, and also fast out-of-band phone-to-network signaling. The rise in mobile phone usage as a result of 2G was explosive and this era also saw the advent of prepaid mobile phones. In 1991, the first GSM network (Radiolinja) launched in Finland. In general, the frequencies used by 2G systems in Europe were higher than those in the United States, though with some overlap. For example, the 900 MHz frequency range was used for both 1G and 2G systems in Europe, so the 1G systems were rapidly closed down to make space for the 2G systems. In the United States, the IS-54 standard was deployed in the same band as AMPS and displaced some of the existing analog channels.
Thank you!
Your vids are the best, no one goes into as much detail as you on TH-cam. I hope more people find your channel
Thank you for clearing all my doubts... I have never understood atmospheric science so well that I understood it through your precise explanations. Loads of thanks from India.🙌
Excellent explanation! Thank you very much!
By some miracle, I am the first to comment on this video.
Thank you very much for making all this material available. Excellent explanation. I am very grateful ❤️
Thank you very much! Excellent explanation 🙏🏽🙏🏽
thank you capt!
Sir , you said weak temp gradient in layer of atmosphere give rise to strong wind. Sir i want to know vertical or horizontal temp gradient?
Sir , I read somewhere that wind speed is greatest were temp difference between air mass is greatest.
Thanks Professor Remer, much help even 8 years later!
In the wind profiler output (around the 7 min mark), data appears not to be plotting in the bottom right (nearest the surface). What could be some typical reasons for this?
Terrific intro. Thank you for posting.
i wish he went into more detain on the last 3 groups of 5 digit numbers
Y'all, what kind of weather system is located in purple during this time period?
hi! where can I find the images you depicted on the presentation? I mean the ones from the main avwather center site. or where can I find the whole document?
Thank you you have helped me a lot...😊
He mentioned that the stall horn won’t sound or show an indication, is it for an specific aircraft? Or is it any way it can happen to a C172?
7 years and still help too many pilots thanks from the heart do this updated ? I found in was book ISOL 4/8th , OCNL more than 4/8th to 6/8th, AC 00-45H
what a wonderful job you did! clearly explained. wonderful materials put together!!! thank you so much
Hello Fred . If you have a power cut and it's raining and your gauge tips 10 times say, will those 10 tips be recorded? Just asking. Jim.
Excellent Explanation. thank you very much
thank you
Time waste
Good content
Nice
I’m not even a pilot but lenticular clouds are my favorite clouds and have been trying to figure out what facilitates these beautiful clouds. What is that a picture of at 8:14?
Ive had many flight instructors try to teach me about steady-state and air mass thunderstorms... with relatively zero success. But you explaining it in terms of "Shear" has helped me tremendously!!! Wow! Thank you so much for this.
why is vorticty maximum on the left of jetstreak
brilliant! much more concrete than what i read on wikipedia… just need to compare and contrast with convection! Thanks!
Lost a friend last year..NTSB sill investigating but I believe this happened (Beechcraft 58 Baron, N585CK)
Thank you for providing a simple and understandable approach to a complex subject!
Nice explanation. what is the sampling time of the radiosonde data?
Thank you! @0:56 But what dahell barble means?
Thank you!
Thank you!
Awesome! Thank you
Very helpful, thank you.
Thanks a lot for this marterial, sir! Isnt the vert. prop. wave the same as the hydraulic jump?
thanks from india
Thanks Sir for These useful Video.Hope to See more in Future...👍👍
This is what happened to all those aircraft crashes in the Nevada triangle, They keep calling it an unknown force but there is nothing unknown about it and here is explained extremely well. In September 2008, a hiker found Steve Fossett's identification cards in the Sierra Nevada Mountains, California, leading shortly thereafter to the discovery of the plane's wreckage. Fossett's only known remains, two large bones, were found half a mile (800 m) from the crash site, probably scattered by wild animals. There were about 2000 aircraft lost in this area and one is rather surprised that all those pilots did risk it to fly in the lee of the mountains. The explanation in this video is excellent. Every pilot should take heed of this information.