Circulation-Best-Of.mp3
Circulation-Best-Of.mp4
Circulation.mp3
Circulation.mp4
Circulation-intro.mp3
[Intro]
(Anticipation)
Depending on the circulation
Caught up in a dream
(Ridin’ the jet stream)
[Verse 1]
Down in the doldrums
Trade winds come undone
The attitude
Of horse latitudes
[Bridge]
(Dream of the scene)
[Chorus]
(Anticipation)
Depending on the circulation
Caught up in a dream
(Ridin’ the jet stream)
[Verse 2]
Currently caught in the current
(Can’t hide from the waves or tide)
Aspire to the gyre (riding higher)
Hey! Thermohaline time (devine)
[Bridge]
(Dream of the scene)
[Chorus]
(Anticipation)
Depending on the circulation
Caught up in a dream
(Ridin’ the jet stream)
[Bridge]
(Dream of the scene)
[Chorus]
(Anticipation)
Depending on the circulation
Caught up in a dream
(Ridin’ the jet stream)
[Outro]
Know what I mean
(Dream of the scene)
Get around
(And get down)
Get down
A SCIENCE NOTE
Chaos theory underscores the intricate, nonlinear, and interconnected nature of the relationships between soil, atmosphere, and oceans in the context of thermal energy and carbon storage. These interactions contribute to the Earth’s climate system’s complexity, and understanding these dynamics is crucial for accurately modeling and predicting climate changes. In addition, thermal energy and carbon are redistributed throughout the world.
Circulation systems of air and/or water include:
* doldrums, trade winds, horse latitudes, prevailing westerlies, polar front zone, and polar easterlies
* each hemisphere has three cells — Hadley cell, Ferrel cell and Polar cell in which air circulates through the entire depth of the troposphere
* usually each hemispheres has two jet streams — a subtropical jet stream and a polar-front jet stream
* waves, tides, currents, downwelling, upwelling move water
* there are over 24 currents — Benguela Current, California Current, Falkland Current, Labrador Current, Brazil Current, Florida Current, Gulf Stream, West Australian Current, Canary Current, Kuroshio Current, North Pacific Current, Somali Current, Antarctic Circumpolar Current, Antarctica Current, Antilles Current, Mozambique Current, North Atlantic Drift, Norwegian Current, Oyashio Current, West Wind Drift, Agulhas Current, South Equatorial Current, Humboldt or Peruvian Current, Monsoon Current
* five major ocean-wide gyres — the North Atlantic, South Atlantic, North Pacific, South Pacific, and Indian Ocean
* thermohaline (temperature and salinity) circulation systems — Gulf Stream, Atlantic Meridional Overturning circulation (AMOC), Pacific Meridional Overturning Circulation (PMOC)
* ocean-atmosphere oscillations — La Nina / El Nino-Southern Oscillation (ENSO), Antarctic Oscillation (AAO), Arctic Oscillation (AO), Atlantic Multidecadal Oscillation (AMO),
Indian Ocean Dipole (IOD), Madden-Julian Oscillation (MJO), North Atlantic Oscillation (NAO), North Pacific Gyre Oscillation (NPGO), North Pacific Oscillation (NPO), Pacific Decadal Oscillation (PDO), Pacific-North American (PNA) Pattern
* Our probabilistic, ensemble-based climate model — which incorporates complex socio-economic and ecological feedback loops within a dynamic, nonlinear system — projects that global temperatures could rise by up to 9°C (16.2°F) within this century. This far exceeds earlier estimates of a 4°C rise over the next thousand years, highlighting a dramatic acceleration in global warming. We are now entering a phase of compound, cascading collapse, where climate, ecological, and societal systems destabilize through interlinked, self-reinforcing feedback loops.
We examine how human activities — such as deforestation, fossil fuel combustion, mass consumption, industrial agriculture, and land development — interact with ecological processes like thermal energy redistribution, carbon cycling, hydrological flow, biodiversity loss, and the spread of disease vectors. These interactions do not follow linear cause-and-effect patterns. Instead, they form complex, self-reinforcing feedback loops that can trigger rapid, system-wide transformations — often abruptly and without warning. Grasping these dynamics is crucial for accurately assessing global risks and developing effective strategies for long-term survival.
Tipping points and feedback loops drive the acceleration of climate change. When one tipping point is toppled and triggers others, the cascading collapse is known as the Domino Effect.
Explore the fundamentals of chaos theory in Edge of Chaos — where order meets unpredictability.
Understand the fundamentals of Statistical Mechanics and Chaos Theory in Climate Science.