Water in the Atmosphere - Chapter 11 Geography NCERT Class 11
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- Опубліковано 5 сер 2024
- Video lecture, lesson summary, revision notes and solutions of CBSE NCERT Geography Class 11 Chapter 11 Water in the Atmospheric. This educational video is important and forms foundation for UPSC / IAS, SSC CGL, CDS, NDA and other school examinations.
**Time Stamp**
1. What is Transpiration? @ 0:36
2. What is Condensation and Precipitation @ 0:54
3. Absolute Humidity @ 3:31
4. Relative Humidity @ 4:25
5. Air Saturation @ 5:14
6. Dew Point @ 7:35
7. Evaporation and Condensation @ 8:35
8. What is Sublimation? @ 9:52
9. Ideal conditions for condensation to take place @ 11:38
10. What is Dew @ 15:13
11. What is Frost @ 16:14
12. What is Fog and Mist @ 16:51
13. What are Clouds and different types of clouds @ 20:49
14. What is Precipitation @ 26:36
15. Types of Rainfall (convectional, orographic, cyclonic rain) @ 27:37
16. World Distribution of Rainfall @ 36:43
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Dear Sir
I saw your Channel Content yesterday and just completed the 11 Chapters which have been explained by you,
Sir the way you have explained each of the terms is phenomenal and trust me these concepts are going to be with me throughout my life.
And its a further request sir if you come up soon with the remaining parts of Chapter 10(CYCLONES)
AND OTHER REMAINING CHAPTERS OF THIS BOOK
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THANKS ALOT AMIT ITS REALLY HELPFUL FOR PEOPLE LIKE ME WHODONTHAVE COACHING CLASS ACCESS & ARE WORKING PRODFESSIONALS &DEPENDENT ON SUCH A RELIABLE COURSE ....THANKS A LOT BUDDY...I WOULD SURELY MEET U ONCE I WILL SUCCEED IN MY EXAM...
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Happy Teacher's Day 🌻
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A great source of information. Thanks for making it simple and comprehensible for us.
I have been so addicted to the way of ur explanation that no other videos seems to make a dent.... So please upload the videos on chapter 10 "extra tropical and tropical cyclones "
Thanks
the knowledge of the subject and the method of teaching is just awesome... the way u delivered the lecture is very much impressive thats make u different from others.
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Really you are blessed with multiple talents to make the viewers to understand .Voice,explanation,examples and all that essentiial are very simple and very clear
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Sir, between 45° and 65° N and S of equator under the influence of westerlies shouldn't the eastern margin receive more rainfall? How is western region receiving more rainfall? @39:12
I have just started following your video since week and I must say that the explanation and the way of explanation is awesome. You have sound knowledge of geography. I have become fan of your teaching. Hat's off for you. I am preparing for UPPSC 2018 AND I learned a lot from your videos. Thank you very much sir. Sir I have a request , If you can make a video for the factual and map based chapters like major river Dam's, Tiger Reserves, Biospheres , All the passes in himalayas and rearranging them in north to south or east to west and lot of these type of map based questions . It will be very helpful to us.
Have you cleared UPSC
Very nice explanation sir
Thnk u
Sir plzz upload other rest chptr also..
Exam is very near...
Plz sir....
Concepts are well defined and your pronunciation is fabulous. A lot of thanks for such great work.
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*U r beyond awesome* yaar.....……!!!
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may you plz make a separate video for teaching how to make such awesome presentation
Himanshu Agrawal i
vacuum means nothing
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not even by magic
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Thank you for the video. Just one query; I think the definition of the latent heat of vaporisation is not correctly given in the book.
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Sir..If condensation takes place in high pressure zone than how it happens in Troposphere where the pressure is low..(Temperature and pressure decreases with increasing in height as you told).
Thnx sir
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Plz make video on last unit remaining part CYCLONE . it will be very helpful
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A hear full thanking to you
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Likha kya h symbol Kon sa dala h
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Hey there, your video is really helpful as an introduction for studying for my climate systems and processes exam. Meteorology master student here :) You just confused me for a second by saying the troposphere was high up, like 12 km in the air or so. That's not correct, the troposphere starts at the ground, always, the tropopause (the upper boundary of the troposphere which separates the troposphere from the stratosphere) is variable, though. When there is convection during the daytime due to solar insolation, it is higher than at night. Why it's like that - you explained in the video :) Cheers from Germany and thank you for the video, will check out your other ones, too! Also, following. And you do have a nice voice! Haha
It really helped me ....
Respected Sir
Sir plz complete this portion
Ur way of explaination is really nice
Sir u skipped important topics like thunderstorms,sleets,extra tropical cyclones...mainly these topics needs more clarifications so if u can upload a video on these topics it would b a great help.. thank u
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Thank you sir .. Sir one request please complete this book soon.. Not much time left for prelims.. Waiting for the next vedio..
Sir you have an amazing teaching skills
Time stamp so useful
Thanks for it