Stefan Becker
Stefan Becker
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Becker Vlog Morocco 2023
Becker Vlog Morocco 2023
Переглядів: 156

Відео

Becker Vlog Israel 2023
Переглядів 61Рік тому
Becker Vlog Israel 2023
Ideas for a 10-day trip to Southern Africa
Переглядів 4915 років тому
Ideas for a 10-day trip to Southern Africa
Manaslu Trek October 2017
Переглядів 22 тис.6 років тому
Impressions of a hike around the Manaslu in Nepal. Information on the region presented in the video was taken from Pritchard-Jones and Gibbons: A Trekking Guide to Manaslu and Tsum Valley (2016)
Chapter 14 Air Masses
Переглядів 4,7 тис.8 років тому
Chapter 14 Air Masses
Chapter 12 Clouds
Переглядів 9 тис.8 років тому
Chapter 12 Clouds
Chapter 21 Climate Change
Переглядів 1,9 тис.8 років тому
Chapter 21 Climate Change
Chapter 1a Solar Energy
Переглядів 5 тис.8 років тому
Chapter 1a Solar Energy
Chapter 23 Human Bioclimatology and the Urban Climate
Переглядів 9508 років тому
Chapter 23 Human Bioclimatology and the Urban Climate
Chapter 15 Midlatitude Cyclones
Переглядів 10 тис.8 років тому
Chapter 15 Midlatitude Cyclones
Chapter 4 Air Temperature
Переглядів 8 тис.8 років тому
Chapter 4 Air Temperature
Chapter 3 Solar Radiation
Переглядів 10 тис.8 років тому
Chapter 3 Solar Radiation
Chapter 6 Global Circulation
Переглядів 6 тис.8 років тому
Chapter 6 Global Circulation
Chapter 5 Air Pressure and Winds
Переглядів 16 тис.8 років тому
Chapter 5 Air Pressure and Winds
Chapter 13 Precipitation
Переглядів 4,9 тис.8 років тому
Chapter 13 Precipitation
Chapter 22 Air Pollution
Переглядів 1,2 тис.8 років тому
Chapter 22 Air Pollution
Chapter 8 Wind Systems
Переглядів 6 тис.8 років тому
Chapter 8 Wind Systems
Chapter 19 Weather Forecast
Переглядів 1,7 тис.8 років тому
Chapter 19 Weather Forecast
Chapter 18 Hurricanes
Переглядів 1,7 тис.8 років тому
Chapter 18 Hurricanes
Chapter 2 The Atmosphere
Переглядів 5 тис.8 років тому
Chapter 2 The Atmosphere
Chapter 16 Thunderstorms
Переглядів 3 тис.8 років тому
Chapter 16 Thunderstorms
Chapter 10 Adiabatic processes, lapse rates and rising air
Переглядів 353 тис.8 років тому
Chapter 10 Adiabatic processes, lapse rates and rising air
Chapter 1b The Seasons
Переглядів 3,7 тис.8 років тому
Chapter 1b The Seasons
Chapter 7 Upper Air Circulation
Переглядів 18 тис.8 років тому
Chapter 7 Upper Air Circulation
Chapter 20 El Nino
Переглядів 2 тис.8 років тому
Chapter 20 El Nino
Chapter 11 Atmospheric Stability
Переглядів 99 тис.8 років тому
Chapter 11 Atmospheric Stability
Chapter 9 Water in the Atmosphere
Переглядів 11 тис.8 років тому
Chapter 9 Water in the Atmosphere
Chapter 17 Tornadoes
Переглядів 1,5 тис.8 років тому
Chapter 17 Tornadoes

КОМЕНТАРІ

  • @nour4828
    @nour4828 5 днів тому

    Thank you so much

  • @socksisdead4098
    @socksisdead4098 9 днів тому

    thanks i love u

  • @captainsxr
    @captainsxr Місяць тому

    Sir ur videos are full of precise & very useful information

  • @nikodeleu3027
    @nikodeleu3027 Місяць тому

    Can you explain why trade winds reverse before an el nino event? Since trade winds are caused by the coriolis force, how can they reverse?

  • @AnkurNautiyal5
    @AnkurNautiyal5 2 місяці тому

    Explained lucidly🙌🏻

  • @robdalsheim4481
    @robdalsheim4481 4 місяці тому

    Thank you Stefan! Now I finally understand thanks to you!

  • @RajivShekhar-un9hm
    @RajivShekhar-un9hm 4 місяці тому

    Superb lecture. So easy to understand. As professor myself, I have a lot to learn from Prof. Becker.

  • @carlbrenninkmeijer8925
    @carlbrenninkmeijer8925 5 місяців тому

    So clear ! It removed some of my cloudy thinking this is excellent !

  • @mitchellkaye9619
    @mitchellkaye9619 5 місяців тому

    I came to this video during preparation for a Sailplane FAA oral exam and checkride. Thank you so much. The content is concise, clear and the illustrations really clarify the material. Best wishes

  • @UgneValantinaviciute
    @UgneValantinaviciute 6 місяців тому

    Great video. I'd like to thank my friend Roisin for keeping me company as I watched it.

  • @MeenuKumari-lh8ps
    @MeenuKumari-lh8ps 6 місяців тому

    Thank you Mr Stefan. These videos are really comprehensive yet precise. Helps building strong conceptual foundation.

  • @robertmcdaniel8147
    @robertmcdaniel8147 6 місяців тому

    If energy is released through condensation, why isn't the process called DIABATIC instead wet adiabatic? Thanks

  • @catvalentine4317
    @catvalentine4317 7 місяців тому

    Incredibly informative! Thank you so much for providing such a well-structured lecture for free! :)

  • @metcas
    @metcas 8 місяців тому

    Exactly what I was looking for, been wanting to formalize my meteorological understanding for a long time. I may consider putting together a playlist for you because the lessons are kind of all over the place chronologically.

  • @RyanMarshburn
    @RyanMarshburn 9 місяців тому

    I fucking hate school. I cant believe I paid money to learn this useless bullshit

  • @michaelaberger6403
    @michaelaberger6403 9 місяців тому

    This explanation is clear! Thank you!

  • @tiloschlumberger
    @tiloschlumberger 10 місяців тому

    still very good contect - thank you!

  • @theskyobserver
    @theskyobserver 11 місяців тому

    Sir, your video is gold.... May I ask where can we access the simulation you use to explain the stability. Thanks

  • @vasu4486
    @vasu4486 Рік тому

    Yes

  • @tombouie
    @tombouie Рік тому

    Good-day, ?Could you place the chapters into a convenient playlist, thks in advance.?

  • @charlessmith263
    @charlessmith263 Рік тому

    Answer to Question 11a - Take a surface temperature of 92 degrees at low levels with a dew point of 73F. It is 2pm - time of peak insolation heating. The high dew point and the surface heating will allow the air parcel to eventually break convective inhibitions in the surface-based environment, discourage sinking, and allow a lapse rate to go up to 7C to 8C per km, which will eventually lead to an air mass thunderstorm, which is the final product of atmospheric instability. Answer to Question 11b - Take a surface temperature of 75 degrees, with a dew point of only 50 degrees. There is full insolation, but with the low dew point reading, the lapse rate will be roughly only 3C to only 4C (maybe 5C per centimeter), and this low level dewpoint means the sinking of air - or subsidence - is very, very strong. Even if there is a moist adiabatic rate that can cause cumulus clouds at the LCL, the low lapse rates will not allow the cumulus to grow any further into thunderstorms. So this is called fair weather cumulus, and this subsidence and low dew points will mean fair or good weather, which will mean the atmosphere is now stable, thanks to the lower lapse rate.

  • @charlessmith263
    @charlessmith263 Рік тому

    Sinking air is known as subsidence.

  • @RajashreeSahoo-g4g
    @RajashreeSahoo-g4g Рік тому

    Thank u sir It is very nice and helpful vedeo .

  • @thenietelhadbeautiful6785

    Please let us your email

  • @thenietelhadbeautiful6785

    Can i contact you please

  • @MaDracula
    @MaDracula Рік тому

    I can't believe this is still helpful after 6years ago, THANK YOU SIR

  • @svensubunitnillson1568
    @svensubunitnillson1568 Рік тому

    Clear and consise. sometimes reading concepts can be hard, but with graphics and clear language you've explained it brilliantly. danke!

  • @Conqurer26
    @Conqurer26 Рік тому

    Very nice explanation love from india❤

  • @eriknijland9818
    @eriknijland9818 Рік тому

    Been there in 1995, some changes in between I saw....

  • @jessalinnguyen1504
    @jessalinnguyen1504 Рік тому

    Thank you so much! This helped me understand

  • @menozmenoz
    @menozmenoz Рік тому

    I'd love to see the rest of the videos that are missing!

  • @grindupBaker
    @grindupBaker Рік тому

    Thanks "pull it upward" at 9:44 S.B. "push it upward". A huge version of the effect at 6:57 is the desert zones nominally latitudes around 30S & 30N. It rises wet from warm ocean in the ITCZ and cools at the moist rate, heads towards Poles, gets turned west--->east by Coriolis Effect and then descends warming at the dry rate with the water latent heat having warmed it on the way up & hot dry air at the surface results, deserts.

  • @nscan22
    @nscan22 Рік тому

    I owe you lots of beers. Thank you.

  • @the81kid
    @the81kid Рік тому

    Very clearly explained. Thanks!

  • @leta3910
    @leta3910 Рік тому

    I understand that when air rises, pressure decreases, volume increases, and temperature decreases through adiabatic cooling. However, I've also been told that cool air contracts like warm air expands. How does that work- wouldn't these two facts balance each other out and the air wouldn't move at all?? Obviously it works out that cold air rises because if I go climb a mountain it will be chillier at the top. But cold air is also more dense than warm air, so how is it higher and how is this true? I feel like adiabatic processes are true to the world but somehow go against those other facts I know.

  • @njchannel8013
    @njchannel8013 Рік тому

    you are so underrated...this is knowledge instead of youtubeknowledge:)

  • @naykia6862
    @naykia6862 Рік тому

    prof Dane Wigington expleins some important details to have a clear idea

  • @porterpotty36Y
    @porterpotty36Y Рік тому

    What book is this video referring to?

  • @kainajones9393
    @kainajones9393 Рік тому

    Finally!!! a clear explanation. Tried wikipedia, and as usual the explanation was written for a postdoc in thermodynamics.

  • @tpstrat14
    @tpstrat14 Рік тому

    So clouds form because the water vapor expands to contract into liquid. Got it 😵‍💫

  • @tpstrat14
    @tpstrat14 Рік тому

    I think i just self diagnosed ADD. I keep thinking a diabatic process is when you eat candy and chips and an adiabatic process is when you eat vegetables. I know this is not what he's talking about but my brain doesn't.

  • @odyssey37
    @odyssey37 Рік тому

    Chinese invasion. Beside that, lovely video with good info and scenery

  • @kimlibera663
    @kimlibera663 Рік тому

    This was informative with good figures to explain these complex processes.

  • @deelofilms
    @deelofilms Рік тому

    12/13/2022, weather pattern matches this video *exactly*

  • @minhduynguyen7351
    @minhduynguyen7351 Рік тому

    this very helpful to me thx

  • @Wawawolfbear
    @Wawawolfbear Рік тому

    These videos are really helpful! Thank you so much Stefan! ^^

  • @shahdhouidi477
    @shahdhouidi477 2 роки тому

    How do we know when it changed from dry adiabatic rate to wet adiabatic rate? i.e. how do we know that happened at 3000 m? How do we calculate that?

  • @nalininanda1976
    @nalininanda1976 2 роки тому

    Thanx alot.U explained it in an easy language without taking much time ,i cud finally understand this topic after searching alot .

  • @bhumibhatt9438
    @bhumibhatt9438 2 роки тому

    it is a very very helpful lacture in short time

  • @shaungorham1871
    @shaungorham1871 2 роки тому

    Cool, Louisiana.