Thank you for the video, could you please help me with a question professor. For internal tides, in vertical mode decomposition, why is mode zero barotropic and mode 1 2 3 and so on baroclinic. Also, can the barotropic and baroclinic mode be in the same fluid at the saem time, how can we picture this? I mean if the ocean stratified? Thank you very much
could you please answer one of my questions? I don't understand why the density of A and B are the same in the barotropic flow(06:44), isn't A and B in the different isopycnic lines?
Tamara， I really like your class so much! thank you so much for sharing these.
Hello sir.. A small doubt
Can you tell me what if Geostrophic wind's path if coriolis parameter was going towards right in the NH?
I don't understand why the density of A and B are the same in the barotropic flow(06:44), isn't that A and B are in the different isopycnic
lines?
❤ nice lecture ❤
Up and to the left? Very confusing
Thanks mam learn alot from here ❤
15:12 You repeatedly said; Temperature controls density. How about pressure, please?
Great video! Thanks
Excellent.
Maam, Can you tell me what if Geostrophic wind's path if coriolis parameter was going towards right in the NH?
Hi Tamara! Could you teach us about geopotential hight related with isobarics surfaces?
Yes it would be really appreciated!
Where do i find the textbook referenced?
Thanks
Nice
That was nice.
Thank you for the video, could you please help me with a question professor. For internal tides, in vertical mode decomposition, why is mode zero barotropic and mode 1 2 3 and so on baroclinic. Also, can the barotropic and baroclinic mode be in the same fluid at the saem time, how can we picture this? I mean if the ocean stratified? Thank you very much
could you please answer one of my questions? I don't understand why the density of A and B are the same in the barotropic flow(06:44), isn't A and B in the different isopycnic lines?