Upending-Upwelling-Best-Of.mp3
Upending-Upwelling-Best-Of.mp4
Upending-Upwelling.mp3
Upending-Upwelling.mp4
Upending-Upwelling-intro.mp3
[Intro]
Upending (Upwelling)
Oh, welling?
[Verse 1]
Climate change causes changes
(In ocean stratification)
Rearranges with multiplication
(Feeding back n’ back n’ back)
[Bridge]
Upending (Upwelling)
Oh, welling?
[Chorus]
So farewell to oh, well
(Upwelling)
To late to sell best not to dwell
(Underwhelming)
Upwelling
[Verse 2]
In fact, the impact on feedback
(Can be overwhelming)
Feeding back n’ back n’ back
(Foretelling the overwhelming of upwelling)
Rendering upwelling underwhelming
(Repeating, repeating, repeating)
[Bridge]
Upending (Upwelling)
Oh, welling?
[Chorus]
So farewell to oh, well
(Upwelling)
To late to sell best not to dwell
(Underwhelming)
Upwelling
[Outro]
So farewell to oh, well
(Upwelling)
To late to sell best not to dwell
(Underwhelming)
Upwelling
A SCIENCE NOTE
Upwelling is a process where deep, cold, and nutrient-rich ocean water rises to the surface, typically replacing surface water that has been moved away by wind or currents. This nutrient-rich water fuels the growth of phytoplankton, which forms the base of the marine food web and supports productive fisheries.
Climate Change Causes Changes in Ocean Stratification
Increased Surface Warming: As the ocean surface warms due to climate change, the water column becomes more stratified, with warmer, less dense water overlying cooler, denser water.
Impact on Upwelling: This stratification can make it more difficult for deep, nutrient-rich water to be brought to the surface by upwelling.
Feedback Loop: While increased upwelling can bring cold water to the surface, surface warming can also enhance stratification, potentially creating a negative feedback loop that limits the effectiveness of upwelling.