Since we now know about upwelling and therefore what areas of the ocean are nutrient rich, a series on fish and fisheries in different locations around the world would connect well to this one
atmospheric circulation pt 3 the wind only affects 1000m when the ocean can go 4000m. thermohailine is what cause currents in the ocean and affect is density. water masses have temp and salinity circulations. the ice cools the surrounding water which cause it to sink as less dense. the water at higher latitudes is too shallow for deep water masses to form. the mediterranean sea receives little precipitation and creates water masses with higher salinity. the ocean conveyor best starts in iceland then goes south with high salinity then moves to antartica then moves to two sections on into the indian and on into north pacific oceans. this belt brings nutrients into these oceans. and they meet back in the north atlantic where the belt began.
Good question! The top of the ocean conveyor belt is the permanent thermocline, which is generally around 500 to 1000m. The thermocline is a result of the well mixed surface waters distributing heat deeper into the water, below the the thermocline the water temperature is much colder. Therefore they don't so much as interact, but really strong surface ocean currents can affect the depth of the thermocline and where the ocean conveyor belt starts. The conveyor belt is also co much weaker compared to the surface ocean currents, so if they were to interact it would result in the conveyor belt being overpowered.
hii mam...your video is very simple and sweet n short.....can you teach me the air- sea interaction ,which are the different processes which occured to air sea interface....
What other series would you like to see us make in the future?
Well, since this video already was about the deep ocean circulation... How about the deep ocean itself? :)
We actually talked about making that a series, after you suggested it as a video! So its in the plans!
Since we now know about upwelling and therefore what areas of the ocean are nutrient rich, a series on fish and fisheries in different locations around the world would connect well to this one
That's a good idea, I always thought a video on how the age of the ocean affects the fish that live there would be interesting too.
Maybe a series about different ocean ecosystems?
what a wonderful presentations.
Hey it is amazing I enjoy this video very much I teach this lesson is properly
"Until next TIDE, I will SEA you later".
I caught that. What a dad pun.
Seriously, great series. I thoroughly enjoyed it.
Glad you enjoyed the series Conrad!
Superb teaching 👍🏻👍🏻👍🏻
Hello This is Prof N.S.Sinha from India,I have watched your video your presentation is excellent,hope to see more interesting video in
future.
Thank you Niladri Singha for the kind words!
Very good teaching I'm learning more from your channel. My name is archit.
Is that really your voice?
Any article abt ocean current of banggai straits ?
Thank you, I am learning a lot from your channel!
Thanks Estudia Feliz, I'm glad you're enjoying them!
atmospheric circulation pt 3
the wind only affects 1000m when the ocean can go 4000m. thermohailine is what cause currents in the ocean and affect is density. water masses have temp and salinity circulations. the ice cools the surrounding water which cause it to sink as less dense. the water at higher latitudes is too shallow for deep water masses to form. the mediterranean sea receives little precipitation and creates water masses with higher salinity. the ocean conveyor best starts in iceland then goes south with high salinity then moves to antartica then moves to two sections on into the indian and on into north pacific oceans. this belt brings nutrients into these oceans. and they meet back in the north atlantic where the belt began.
Thank you very much for this video! ! :)
Glad it was helpful!
As always, wonderfully explained!
Can you please share the link of the other two videos of this series mam?
We have these videos in a playlist here if you would like to watch the others🙂 Ocean Currents: ruclips.net/p/PLLICVSd-zkPgd-LKkrCgOPIlUWSpYnFGs
@@DivingWithMatt Thank you.
@@sukanyachaube4770 your welcome 🙂
Very informative
What is the depth of the Great Ocean Conveyor Belt after it up-wells and does it interact with the surface ocean currents at all?
Good question! The top of the ocean conveyor belt is the permanent thermocline, which is generally around 500 to 1000m. The thermocline is a result of the well mixed surface waters distributing heat deeper into the water, below the the thermocline the water temperature is much colder. Therefore they don't so much as interact, but really strong surface ocean currents can affect the depth of the thermocline and where the ocean conveyor belt starts. The conveyor belt is also co much weaker compared to the surface ocean currents, so if they were to interact it would result in the conveyor belt being overpowered.
hii mam...your video is very simple and sweet n short.....can you teach me the air- sea interaction ,which are the different processes which occured to air sea interface....