Tag: climate chamge

bookmark_borderCirculation

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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.

 

From the album “Lofty“

bookmark_borderSteam

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Steam-I.mp3
Steam-I.mp4
Steam-II.mp3
Steam-II.mp4
Steam-intro.mp3

[Verse 1]
If I’m seeming sad…
(No!) I’m steaming mad
You say sensible heat
(No!) This heat is beat

[Chorus]
I mean the steam
Is a gas
Shattered the dream
Pass to past

[Verse 2]
Vaporization
Causes hesitation
In my thought process

[Verse 3]
Current situation
Clausius-Clapeyron relation
Saturation… more or less

[Chorus]
I mean the steam
Is a gas
Shattered the dream
Pass to past

[Bridge]
Be forewarned (of the storm)
Positive feedback (attack)
Exponentially (inevitability)
Delivers (atmospheric rivers)
Hurricane (going insane)
Heatwaves (nothing saves)

[Chorus]
I mean the steam
Is a gas
Shattered the dream
Pass to past

[Outro]
Be forewarned (of the storm)
Positive feedback (attack)

A SCIENCE NOTE

A burn from steam is generally more severe than a burn from boiling water because of the additional energy stored in steam as latent heat—a concept rooted in thermodynamics and phase changes.

Here’s a breakdown of the physics:

1. Boiling Water: Sensible Heat

  • Boiling water at 100 °C (212 °F) contains sensible heat—the energy required to raise its temperature from room temperature to 100 °C.

  • When this hot water contacts skin, it transfers that thermal energy directly to the tissue, causing a burn.

2. Steam: Latent Heat of Vaporization

  • Steam is water in its gas phase, also at 100 °C, but it contains extra energy beyond just being hot.

  • This extra energy is called the latent heat of vaporization: the energy required to convert liquid water to steam at the same temperature.

    • For water, this is about 2260 kJ/kg, which is over five times the energy required to heat water from 0 °C to 100 °C.

  • When steam contacts your skin, it condenses back into liquid water—and in doing so, it releases all that latent heat into your skin.

3. Why It Hurts More

  • So steam at 100 °C can deliver both:

    • The thermal energy from its temperature (same as boiling water), plus

    • The latent heat from condensing back to water.

  • This double dose of heat energy causes deeper tissue damage in a shorter time.

This concept of latent heat—the same reason steam burns are worse—has direct parallels in climate change, especially regarding extreme weather and the water cycle.

How It Relates to Climate Change:

1. Warmer Atmosphere = More Water Vapor

  • A warmer atmosphere holds exponentially more water vapor (about 7% more per 1°C of warming) due to the Clausius-Clapeyron relation.

  • Water vapor is itself a greenhouse gas, reinforcing warming (positive feedback).

2. More Latent Heat in the System

  • As water evaporates from oceans, lakes, and soil, it stores latent heat—just like steam.

  • When this vapor condenses (in clouds, storms, hurricanes), it releases latent heat, supercharging storms by:

    • Intensifying updrafts in thunderstorms.

    • Powering hurricanes and cyclones.

    • Driving heavier rainfall and flash floods.

3. Steam Burn Analogy

  • Just like condensing steam transfers a massive amount of energy to your skin, condensing atmospheric moisture transfers massive energy to the atmosphere.

  • This leads to more violent weather, akin to the difference between being splashed by boiling water and burned by steam.

Real-World Impacts:

  • Hurricanes: Stronger and wetter due to latent heat release and increased water vapor.

  • Atmospheric Rivers: Carry more moisture, dumping extreme rainfall.

  • Heatwaves + Humidity: Higher latent heat content makes nights hotter and reduces cooling.

Summary:

Latent heat acts like hidden energy in the climate system—just as it makes steam burns worse, it makes storms and extreme weather more powerful in a warming world.

From the album “To Too Hot“

The Human Induced Climate Change Experiment