Category: Business

bookmark_borderAbout the Membrane Domain

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This website was established by a diverse group, including musicians, writers, computer wizards, businessmen, videots, and individuals with a keen interest. We named this collective effort “The Philadelphia Spirit Experiment.”

PHILADELPHIA? Frustrated with outdated systems and unsuccessful attempts to change them, we chose to take action — perhaps in the spirit of our forefathers?

SPIRIT? The aim of the spirit experiment is to leverage R&D (research and development of business/art/science models) to directly contribute to preserving mankind. Can we help reintroduce the “kind” into mankind by replacing formalized formulas? Our goal is to infuse life with spirit.

Our climate model employs chaos theory to comprehensively consider human impacts and projects a potential global average temperature increase of 9℃ above pre-industrial levels. Global warming is a consequence of elevated thermal energy in the climate system, which comprises various subsystems. Chaos theory underscores the intricate and nonlinear nature of dynamic systems. Human well-being is compromised above a 1.5-degree temperature rise, rendering much of the Earth uninhabitable. A 9-degree Celsius increase would bring the Earth close to a wet-bulb temperature incapable of sustaining human life.

What Can I Do? There are numerous actions you can take to contribute to saving the planet. Each person bears the responsibility to minimize pollution, discontinue the use of fossil fuels, reduce consumption, and foster a culture of love and care. The Butterfly Effect illustrates that a small change in one area can lead to significant alterations in conditions anywhere on the globe. Hence, the frequently heard statement that a fluttering butterfly in China can cause a hurricane in the Atlantic. Be a butterfly and affect the world.

What you can do today. How to save the planet.

A RADICAL APPROACH? Our approach draws on past experiences to make the present count for tomorrow—a radical notion, albeit one focused on positive change.

This concept is put into action (or lack of action) through music, publishing, business, moving pictures, and more. The original idea gained popularity, leading to the development of a domain centered around altruism.

Whether you choose to participate or simply educate yourself, we hope your time here is enjoyable at The Membrane Domain.

The web is an extension of our dynamic approach — it is alive. Each visit can offer a completely different experience. Please feel free to explore as often as you like. If you encounter bad “links” or spelling errors, we appreciate your feedback.

Should you need assistance during your visit, click on PANIC! / PANIC! to connect with a human. Regardless of your issue or question, don’t hesitate to reach out.

Thank you for your attention. We hope you grasp the essence of our intentions. If you’re ready, enter the Lyon’s Den — the labyrinth of the Membrane Domain.

Sincerely,
C. Moore
Philosopher

bookmark_borderEarth’s Vital Signs

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by Daniel Brouse

Earth
Earth

Human-induced climate change serves as a dynamic and intricate component within an unordered system, guided by chaos theory. This suggests that global warming is undergoing exponential acceleration in a complex manner. The pace at which climate change is accelerating can be described as rapid, as evident in the intensity, duration, and likelihood of climate disasters. Drawing insights from the 2023 Canada wildfires, the World Weather Attribution Organization reported, “Climate change made the cumulative severity of Quebec’s 2023 fire season to the end of July around 50% more intense, and seasons of this severity at least seven times more likely to occur.”

Key Findings: Extreme weather and climate-related disasters have become 50% more intense and 7 times more likely.

In the 20th century, Earth’s surface temperature averaged 13.9℃. However, in the initial weeks of July 2023, the average temperature surged to 17℃. Human activities have propelled global temperatures more than 3℃ for parts of the year, with the entire period from February 2023 to February 2024 registering 1.5℃ above pre-industrial levels. A rise of 1.5 degrees already compromises human well-being, making much of the Earth uninhabitable.

As of 2024, humanity has surpassed seven critical tipping points, including Mountain Glacier Loss, Greenland Ice Sheet Collapse, Antarctic Ice Sheet Collapse, AMOC (Atlantic Meridional Overturning Circulation) Collapse, Amazon Rainforest Dieback, Coral Reef Die-Off, and Northern Permafrost Collapse. Crossing these tipping points triggers self-sustaining feedback loops independent of human activity. While the exact carbon stored in nature remains uncertain, an assumption could be made that temperatures might surge from 3 to 6 degrees above pre-industrial levels. Thriving beyond a 1.5-degree rise becomes impossible for humans. If an additional 3 degrees Celsius is added, the temperature and humidity would approach a wet-bulb temperature unsuitable for human life.

What Can I Do?
There exist numerous actions individuals can take to contribute to saving the planet. Each person bears the responsibility to minimize pollution, discontinue the use of fossil fuels, reduce consumption, and foster a culture of love and care. The Butterfly Effect illustrates that a small change in one area can lead to significant alterations in conditions anywhere on the globe. Hence, the frequently heard statement that a fluttering butterfly in China can cause a hurricane in the Atlantic. Be a butterfly and influence the world.

The Human Induced Climate Change Experiment

bookmark_borderClimate Change: What Can I Do?

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by Daniel Brouse and Sidd Mukherjee

Achieving “net zero” is not only accessible but also cost-effective, providing substantial savings while contributing to the preservation of our planet. Here are some practices I’ve adopted to reach net zero without compromising my standard of living, and, in fact, surpassing it in an effort to eliminate all my pollution. The simplest way to commence this journey is through energy conservation. Be mindful of your energy usage, refrain from unnecessary consumption, turn off devices when not in use, and opt for low-energy products.

  1. Consume less. Consumer habits have played a significant role in damaging the world’s environment and economies. The insatiable demands of mass consumption have led to the exploitation of natural resources and the emission of pollution and greenhouse gases. In many instances, it’s feasible to choose not to consume certain products entirely. Travel, fashion, and meat are examples of areas where consumption could be minimized. Reducing overall consumption is the most impactful individual contribution towards eliminating pollution and mitigating the effects of climate change. The critical aspect of reducing consumption is to cease burning fossil fuels and using hydrocarbon products immediately. (Hydrocarbons encompass plastics, polymers, petroleum, and natural gas.)
  2. Electricity and heat are leading contributors to greenhouse gas emissions.
  • Select an electric company that relies on nuclear, solar, and/or wind generation.
  • Insulate your house (Be cautious not to over-insulate, as indoor pollution can be as concerning as outdoor pollution. An air-tight house requires an air exchange system with a meticulous filter maintenance program.)
  • Zone heat: In winter, maintain your main temperature at 50 degrees Fahrenheit and only heat the room you are occupying to a comfortable level (e.g., 68 degrees). Dress warmly.
  • Install an air-to-air heat exchanger and humidity exchanger (Note: Humidity is as crucial as temperature.)
  • Plant shade trees to reduce the need for central air.
  • Plant windscreens, such as evergreens.
  1. Food and land use constitute the second-largest contributors to greenhouse gas emissions.
  • Consume less meat.
  • Minimize the transportation of food by choosing local products.
  • Cultivate your own garden and windowsill gardens.
  • Plant trees, with a focus on preserving old-growth.
  • Reduce impervious surfaces.
  1. Transportation represents the third-largest contributor to greenhouse gas emissions.
  • Purchase an electric vehicle (EV) or a high MPG manual transmission vehicle (I achieve 50 MPG in a 4-wheel drive SUV with a 6-speed.)
  • Make fewer trips, use public transportation, and minimize air travel.

* Our climate model employs chaos theory to comprehensively consider human impacts and projects a potential global average temperature increase of 9 degrees Celsius above pre-industrial levels.

What Can I Do?
There are numerous actions you can take to contribute to saving the planet. Each person bears the responsibility to minimize pollution, discontinue the use of fossil fuels, reduce consumption, and foster a culture of love and care. The Butterfly Effect illustrates that a small change in one area can lead to significant alterations in conditions anywhere on the globe. Hence, the frequently heard statement that a butterfly in China can cause a hurricane in the Atlantic. Be a butterfly and affect the world.
Here is a list of additional actions you can take.

bookmark_borderClimate Change Wildfires

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by Daniel Brouse and Sidd Mukherjee

About the 2023 wildfires in Hawaii, Governor Josh Green said, “For perspective, we’ve had six fire emergencies this August, we had six fire emergencies between 1953 and 2003. That’s how- how fast things are changing. I know that there is debate out there whether we should be talking about climate change or not. Well, let’s be real world, climate change is here we are in the midst of it with a hotter planet, and fiercer storms.”

Climate change is contributing to the increased intensity and frequency of wildfires through a combination of factors that create favorable conditions for wildfires to ignite, spread, and become more destructive. Here are some key ways in which climate change influences wildfires:

  1. Higher Temperatures:
    • Impact: Rising global temperatures increase the likelihood of extreme heat events.
    • Effect on Wildfires: Higher temperatures contribute to drier conditions, leading to increased evaporation and moisture loss from vegetation. Dry and hot conditions provide a more conducive environment for wildfires to ignite and spread.
  2. Drought Conditions:
    • Impact: Changes in precipitation patterns and prolonged droughts are linked to climate change.
    • Effect on Wildfires: Drought conditions result in dry vegetation, making it more susceptible to ignition. Reduced soil moisture levels also contribute to the flammability of ecosystems.
  3. Changing Rainfall Patterns:
    • Impact: Climate change alters regional rainfall patterns, leading to more intense rainfall in some areas and prolonged dry spells in others.
    • Effect on Wildfires: Areas experiencing reduced rainfall may face prolonged dry seasons, creating conditions favorable for wildfires. Intense rainfall in certain regions can lead to the growth of vegetation, which later dries out and becomes potential fuel for fires.
  4. Warming Winters:
    • Impact: Warmer winter temperatures can affect snowpack and contribute to earlier snowmelt.
    • Effect on Wildfires: Reduced snowpack and earlier snowmelt can result in drier soil and vegetation earlier in the year, extending the wildfire season and increasing the period of vulnerability to fire ignition.
  5. Extended Fire Season:
    • Impact: Changes in climate contribute to longer and more intense fire seasons.
    • Effect on Wildfires: A longer fire season means that conditions conducive to wildfires persist for a more extended period, increasing the likelihood of ignition and the potential for wildfires to become larger and more destructive.
  6. Insect Infestations:
    • Impact: Warmer temperatures allow for the proliferation of certain insects, such as bark beetles.
    • Effect on Wildfires: Insect-infested trees become more susceptible to disease and wildfire. Dead and dry trees contribute to the fuel load, increasing the intensity and spread of wildfires.
  7. Wind Patterns:
    • Impact: Changes in climate can influence wind patterns.
    • Effect on Wildfires: Changes in wind patterns can contribute to the rapid spread of wildfires. Strong winds can carry embers over long distances, leading to the ignition of new areas.
  8. Thawing Permafrost:
    • Impact: Warming temperatures contribute to the thawing of permafrost.
    • Effect on Wildfires: Thawing permafrost releases stored carbon, creating flammable conditions. It can also lead to changes in vegetation types, altering fuel availability for wildfires.

The combination of these factors creates a feedback loops, where more intense and frequent wildfires release large amounts of carbon dioxide into the atmosphere, contributing to further climate change. This cycle reinforces the importance of addressing both the causes and consequences of climate change to mitigate the impact on wildfire risk. While the beautiful sunsets during forest fires create captivating visuals, it’s essential to recognize the environmental and health impacts associated with wildfires. Wildfires can cause significant damage to ecosystems, contribute to air pollution, and pose risks to human health. The mesmerizing sunsets are a visible reminder of the interconnectedness of atmospheric processes and the far-reaching effects of natural events like wildfires.

In addition to the carbon feedback loop (the carbon emissions of Canada’s fires outweighed the combined emissions from its oil and gas, transport and agriculture sectors), the fires also cause the melting of the permafrost and zombie fires to burn in the permafrost. The permafrost collapse is a self-sustaining feedback loop/tipping point. As the permafrost melts, the peatlands emit CO2 and methane. The increase in CO2 and methane results in more warming that results in more peatland emissions. A third feedback loop is created with lightning strikes. The study Forests at Risk Due to Lightning Fires found a sensitivity of extratropical intact forests to potential increases in lightning fires, which would have far-reaching consequences for terrestrial carbon storage and biodiversity. The results show that, on a global scale, lightning is the primary ignition source of fires in temperate and boreal forests. Global warming causes more extreme weather events and conditions for lightning creating more forest fires that create more warming and more lightning strikes.

The study Wildfire as a major driver of recent permafrost thaw in boreal peatlands published in the Journal Nature Communications found wildfires have caused a quarter of permafrost thaw (2,000 square kilometres) in Western Canada’s boreal peatlands over the past 30 years. “Historically, permafrost in this area underwent a natural cycle of thawing and reforming, but given current climate conditions and projections for the future, this fire-induced thaw appears to be irreversible,” said Carolyn Gibson, who conducted the research.

On January 1, 2024, the article, Why Are Alaska’s Rivers Turning Orange?, was published in Scientific America. “Streams in Alaska are turning orange with iron and sulfuric acid. Scientists who have studied these rusting rivers agree that the ultimate cause is climate change. Kobuk Valley National Park has warmed by 2.4 degrees Celsius (4.32 degrees Fahrenheit) since 2006 and could get another 10.2 degrees C hotter by 2100, a greater increase than projected for any other national park. The heat may already have begun to thaw 40 percent of the park’s permafrost, the layer of earth just under the topsoil that normally remains frozen year-round. McPhee wanted to protect the Salmon River because humans had ‘not yet begun to change it.’ Now, less than 50 years later, we have done just that. The last great wilderness in America, which by law is supposed to be ‘untrammeled by man,’ is being trammeled from afar by our global emissions.”

NASA reported: Wildland fire experts have described Canada’s 2023 fire season as record-breaking and shocking. Over the course of a fire season that started early and ended late, blazes have burned an estimated 18.4 million hectares. Hundreds of fires exceeded 10,000 hectares (39 square miles), large enough to be considered “megafires.” These megafires were also unusually widespread this season, charring forests from British Columbia and Alberta in the west to Quebec and the Atlantic provinces in the east to the Northwest Territories and the Yukon in the north.

Though the rate of change in climate disasters’ intensity, duration, and likelihood vary according to the type of extreme weather, a “rule-of-thumb” can be derived from the Canada wildfires of 2023. The World Weather Attribution Organization found, “Climate change made the cumulative severity of Quebec’s 2023 fire season to the end of July around 50% more intense, and seasons of this severity at least seven times more likely to occur.”

50% more intense
7 x more likely

Sidd said, “Do you remember back in the early 2000’s when we thought we wouldn’t live to see the extreme changes due to global warming?”

Daniel replied, “I think 2023 is the most significant year so far. We saw confirmation of tipping points being crossed for Mountain Glacier Loss, Greenland Ice Sheet Collapse, Antarctic Ice Sheet Collapse, and potentially the Collapse of AMOC.”

Sidd continued, “We already knew that. It was Canada catching on fire that I could not believe. I never thought I’d live to see the day.”

Daniel asked, “Do you think the permafrost and peatlands will have zombie fires and cause the permafrost tipping point?”

Sidd responded, “Yes. They are gone, too. We already know from the permafrost peatland fires in Siberia.”

Daniel ponders, “Hmmmm… I guess that means my plan went up in smoke? My worst case scenario / last resort emergency plan was to escape to Canada.”

ALSO SEE:
How is All Real Estate at Risk From Climate Change? Brouse and Mukherjee (2024)
The Long-term Breathing Experiment / Brouse (2023)
Health Impacts of Air Pollution / Brouse (2023)
Climate Change: Rate of Acceleration / Brouse and Mukherjee (2023)
Toppled Tipping Points: The Domino Effect / Brouse and Mukherjee (2023)
Tree Extinction Due to Human Induced Environmental Stress / Mukherjee and Brouse (2005)
Soil Degradation and Desertification / Brouse (2024)
Create a Climate-Resilient Environment in and Around Your Home / Brouse (2024)

 

bookmark_borderHow is All Real Estate at Risk From Climate Change?

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By Daniel Brouse and Sidd Mukherjee

Climate change poses risks to real estate in the United States in various ways, and these risks can affect property values, insurance costs, and overall property resilience. Here are some ways in which all US real estate is at risk from climate change:

  1. Sea Level Rise and Coastal Properties:
    • Coastal properties are particularly vulnerable to sea level rise, storm surges, and coastal erosion. As sea levels continue to rise due to global warming, properties near coastlines may experience increased flooding and damage from more frequent and severe storms. Storm surges in Florida are an example.
  2. Extreme Weather Events:
    • Climate change is contributing to an increase in the frequency and intensity of extreme weather events, such as hurricanes, wildfires, floods, and droughts. Properties in regions prone to these events are at risk of damage, destruction, and increased insurance costs.
  3. Temperature Extremes:
    • Rising temperatures can lead to more frequent and prolonged heatwaves, affecting property infrastructure, energy demand, and potentially decreasing property values in areas with extreme heat.
  4. Changes in Precipitation Patterns:
    • Changes in precipitation patterns, including increased violent rainfall or prolonged droughts, can impact properties by causing flooding, landslides, or water scarcity. These changes may affect property values and increase maintenance costs.
  5. Wildfires:
    • Increased temperatures and changing precipitation patterns contribute to the risk of wildfires. Properties in wildfire-prone areas face threats to both their physical structures and the surrounding environment.
  6. Homeowners and Flood Insurance Costs:
    • Flood insurance will become expensive and difficult to obtain. Climate-related risks can lead to higher insurance premiums and deductibles, particularly in high-risk areas. As the frequency and severity of climate-related events increase, insurance companies may reassess risk models and adjust pricing accordingly.
  7. Infrastructure Vulnerability:
    • Climate change can impact infrastructure such as roads, bridges, and utilities. Properties relying on vulnerable infrastructure may face challenges related to accessibility, reliability, and potential increases in repair and maintenance costs.
  8. Health Risks:
    • Humans will experience greater loss and damage to life and quality of life from air pollution, decreasing supply of potable water, extreme weather events, and disease. The greatest short term climate change risk to human health is deadly humid heat (wet-bulb temperature). Climate change can affect human health, and properties in areas prone to heatwaves, air pollution, or vector-borne diseases may face increased health risks. This could influence property values and community desirability.Almost all survivors of climate-related disasters suffer from mental distress. Of those who have not experienced climate disasters, more than two-thirds of U.S. adults (68%) have reported climate change anxiety.
  9. Regulatory Changes:
    • Governments may implement stricter building codes, zoning regulations, and disclosure requirements related to climate-related risks. Non-compliance could affect property values and lead to increased costs for property owners. Loss and damage litigation against oil companies and governments will change world economics.
  10. Shifts in Property Demand:

It’s important to note that the degree of risk varies by region and property type. Some areas may experience more immediate and severe impacts, while others may be more resilient. Assessing and mitigating these risks require a comprehensive understanding of local climate vulnerabilities and the implementation of strategies to enhance property resilience. Policymakers, real estate professionals, and property owners are increasingly recognizing the importance of addressing climate risks to ensure the long-term sustainability and value of real estate assets. Thus, our recommendation to evacuate Florida now (i.e. Managed Retreat).

Create a Climate-Resilient Environment in and Around Your Home Brouse (2024)

Managed Retreat: Relocating Due to Climate Change Extreme Weather Events Brouse (2023)

Stormwater Runoff Management for Your House Brouse (2024)

Tree Extinction Due to Human Induced Environmental Stress Mukherjee and Brouse (2005-present)

Soil Degradation and Desertification Brouse (2024)

Atmospheric Rivers Mukherjee and Brouse (2022-2023)

Violent Rain and the Substrate Brouse and Laden (2024)

The Long-term Breathing Experiment Brouse (2023)

Health Impacts of Air Pollution Brouse (2023)

Plymouth Meeting, Pennsylvania and the Substrate Daniel Brouse (2023)

Real Estate Underwater: A Florida Climate Change Case Study Daniel Brouse (2023)

Climate Change Impacts on Flood Risks and Real Estate Values Sidd Mukherjee and Daniel Brouse (2023)

Real Estate and Climate Change: Stranded on an Island Daniel Brouse (2023)

Tipping Cascades, Social-Ecological Systems, and the Hottest Year in History Brouse (2024)

All About Flood Insurance Brouse and Mukherjee (1995-present)

The Age of Loss and Damage Brouse (2023)

bookmark_borderChaos Theory: Soil, Atmosphere and Ocean Interaction With Thermal Energy and Carbon Storage

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by Daniel Brouse

Chaos theory emphasizes the complexity and nonlinearity of dynamic systems, and this complexity is inherent in the interactions between soil, atmosphere, and oceans in the Earth’s climate system. Here’s how these components interact with thermal energy and carbon storage:

Soil-Atmosphere Interaction:

  1. Thermal Energy Exchange:
    • Soil plays a crucial role in the exchange of thermal energy with the atmosphere. The temperature of the soil surface affects the transfer of heat to the atmosphere through processes such as conduction and convection. The thermal properties of soil, including its composition and moisture content, influence this energy exchange.
  2. Carbon Storage and Cycling:
    • Soil acts as a reservoir for carbon in the form of organic matter. This carbon storage is dynamic and involves complex interactions between plants, microorganisms, and the soil matrix. Soil organic carbon contributes to the global carbon cycle, affecting atmospheric CO2 concentrations.
  3. Feedback Mechanisms:
    • Nonlinear feedback mechanisms between soil and atmosphere can influence climate dynamics. For example, changes in temperature and precipitation patterns may impact soil moisture, affecting vegetation growth and altering the surface energy balance.

Soil-Ocean Interaction:

  1. Carbon Storage and Sequestration:
    • Oceans play a crucial role in global carbon storage. Dissolved carbon dioxide is absorbed by the ocean, forming carbonic acid. Additionally, organic matter from marine life contributes to carbon storage in ocean sediments. The exchange of carbon between soil and oceans is interconnected and can influence atmospheric CO2 levels.
  2. Thermal Inertia:
    • Oceans have a high thermal inertia, meaning they can absorb and store large amounts of heat. This property moderates temperature extremes, influencing atmospheric temperature patterns. Changes in ocean temperatures can, in turn, impact regional and global climate dynamics.
  3. Ocean Circulation and Climate:
    • Ocean circulation patterns, such as the Atlantic Meridional Overturning Circulation (AMOC), play a role in redistributing heat around the globe. Changes in ocean circulation can have cascading effects on atmospheric circulation patterns, influencing climate on a large scale.

Atmosphere-Soil-Ocean Coupling:

  1. Teleconnections:
    • Chaos theory recognizes the concept of teleconnections, where seemingly unrelated events in one part of the Earth system influence conditions in another. For instance, changes in sea surface temperatures (linked to ocean dynamics) can affect atmospheric circulation patterns, leading to variations in precipitation and temperature on land.
  2. Climate Variability:
    • The complex interactions between soil, atmosphere, and oceans contribute to climate variability. Chaos theory helps to understand the sensitivity of the climate system to initial conditions and how small perturbations in one component can lead to significant and sometimes unpredictable outcomes.

In summary, 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. Ongoing research and improved modeling techniques aim to enhance our understanding of these complex interactions and their implications for climate variability and change.

Chaos Theory and Climate Change Brouse (2024)

Climate Change: Rate of Acceleration Brouse and Mukherjee (2023)

Toppled Tipping Points: The Domino Effect Brouse and Mukherjee (2023)

The Human Induced Climate Change Experiment

bookmark_borderClimate Change and How Soil Degradation Can Lead to Desertification

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Why is soil integral to climate change? How does soil degradation lead to desertification?

Soil plays a crucial role in climate change mitigation and adaptation, and soil degradation can contribute to the process of desertification. Here’s why soil is integral to climate change and how soil degradation can lead to desertification:

Importance of Soil in Climate Change:

  1. Carbon Sequestration:
    • Healthy soils act as a significant carbon sink, storing large amounts of carbon in the form of organic matter. This process, known as carbon sequestration, helps mitigate climate change by reducing the concentration of greenhouse gases, particularly carbon dioxide (CO2), in the atmosphere.
  2. Water Regulation:
    • Soil influences water availability and regulates the water cycle. Healthy soils absorb and store water, reducing the risk of floods and contributing to moisture availability during dry periods. This capacity for water regulation is crucial for climate resilience.
  3. Biodiversity Support:
    • Healthy soils provide habitat and support for a diverse range of organisms, including bacteria, fungi, insects, and plant roots. Biodiversity in the soil contributes to ecosystem stability, resilience, and adaptation to changing environmental conditions.
  4. Nutrient Cycling:
    • Soil is essential for nutrient cycling, as it hosts microbial communities that break down organic matter and make nutrients available to plants. This nutrient cycling supports plant growth and contributes to overall ecosystem health.

Soil Degradation and Desertification:

  1. Erosion:
    • Soil degradation, often caused by factors like deforestation, overgrazing, and unsustainable agricultural practices, can lead to increased soil erosion. Erosion removes the topsoil layer, which is rich in organic matter and nutrients, reducing the soil’s fertility and water retention capacity.
  2. Loss of Soil Structure:
    • Poor land management practices, such as excessive plowing, deforestation, and improper irrigation, can lead to the loss of soil structure. This makes the soil more susceptible to erosion, reduces water infiltration, and hinders the growth of vegetation.
  3. Decreased Carbon Sequestration:
    • Soil degradation results in the loss of organic matter, reducing the soil’s ability to sequester carbon. This can contribute to increased atmospheric CO2 levels, exacerbating the greenhouse effect and climate change.
  4. Loss of Biodiversity:
    • Degraded soils often experience a decline in microbial and plant diversity. This loss of biodiversity weakens the soil’s resilience to environmental stresses and reduces its capacity to support healthy ecosystems.
  5. Increased Vulnerability to Climate Change:
    • Degraded soils are more vulnerable to the impacts of climate change, such as extreme weather events, droughts, and temperature variations. This vulnerability can create a feedback loop, where climate change further exacerbates soil degradation.
  6. Desertification:
    • Desertification is the process by which fertile land becomes increasingly arid and unproductive, eventually turning into desert-like conditions. Soil degradation, through erosion, loss of organic matter, and reduced water retention, is a key driver of desertification.
  7. Impact on Livelihoods:
    • Desertification poses a threat to agricultural productivity, water resources, and local livelihoods. It can lead to the displacement of communities and exacerbate social and economic challenges, contributing to a cycle of poverty and environmental degradation.

Addressing soil degradation is crucial for sustainable land management, climate change mitigation, and the prevention of desertification. Implementing conservation practices, agroforestry, reforestation, and sustainable agriculture techniques can help restore and protect soils, contributing to climate resilience and biodiversity conservation.

The Human Induced Climate Change Experiment

bookmark_borderClimate-Resilient Environment Around Your Home

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by Daniel Brouse

Soil is integral to our climate.

What are the best methods to mitigate against climate change by providing wind breaks, shade, moisture retention, and climate control, around my home, as well as prevent soil degradation and desertification?

Creating a sustainable and climate-resilient environment around your home involves a combination of practices that address wind breaks, shade, moisture retention, climate control, and prevention of soil degradation. Here are some effective methods:

  1. Planting Trees and Vegetation:
    • Wind Breaks and Shade: Planting windbreaks, such as rows of trees or shrubs, can protect your home from strong winds and provide shade. Deciduous trees strategically placed on the south and west sides of your home can offer shade during hot seasons while allowing sunlight through during colder seasons.
    • Moisture Retention: Trees and vegetation help retain moisture in the soil by reducing evaporation. Mulching around plants and trees further aids in moisture retention.
    • Climate Control: Trees act as natural air conditioners, cooling the surrounding environment through a process called transpiration. This can contribute to a more comfortable microclimate around your home.
  2. Rainwater Harvesting:
    • Install rain barrels or cisterns to collect rainwater. This harvested water can be used for watering plants, reducing the need for additional irrigation and helping with moisture retention in the soil.
  3. Appropriate Plant Selection:
    • Choose native or drought-resistant plants that are well-suited to your local climate. These plants typically require less water, contribute to soil stability, and are more resilient in the face of climate variability.
  4. Contour Planting and Terracing:
    • Contour planting involves planting along the contour lines of the land to slow down water runoff, promoting infiltration and reducing soil erosion. Terracing is another method to control water runoff on sloped terrain.
  5. Ground Cover and Cover Crops:
    • Planting ground cover or cover crops helps prevent soil erosion, improves moisture retention, and contributes to overall soil health. These plants protect the soil surface from the impact of raindrops and enhance soil structure.
  6. Permeable Surfaces:
    • Use permeable surfaces, such as permeable pavers or gravel, in areas around your home. This allows rainwater to infiltrate into the soil rather than running off, contributing to soil moisture and preventing erosion.
  7. Composting:
    • Implement composting practices to improve soil structure and fertility. Healthy soils are more resistant to erosion, and they can retain moisture better, promoting plant growth.
  8. Integrated Pest Management (IPM):
    • Practice IPM techniques to manage pests without resorting to excessive use of pesticides. Healthy ecosystems are more resilient to climate stresses, and minimizing chemical inputs helps maintain biodiversity and soil health.
  9. Microclimate Planning:
    • Plan your landscaping to create microclimates around your home. For example, placing hard surfaces like rocks or pavement near the home can absorb and release heat, contributing to temperature regulation.
  10. Educate and Involve the Community:
  • Collaborate with neighbors and community members to implement sustainable practices collectively. Building awareness and working together can have a more significant impact on preventing soil degradation and desertification.

By integrating these practices, you can contribute to a more sustainable and climate-resilient environment around your home while mitigating the impacts of climate change and promoting soil health.

The Human Induced Climate Change Experiment

bookmark_borderClimate Change, the Jet Stream, and East Coast Atmospheric Rivers

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by Daniel Brouse

How is climate change impacting the jet stream and atmospheric rivers on the East Coast of the USA?

The interactions between various factors, including ocean currents, sea surface temperatures, and atmospheric circulation, contribute to the overall climate patterns experienced on the East Coast.

Climate change can influence the jet stream and atmospheric rivers, impacting weather patterns on the East Coast of the USA. Here are some key ways in which these changes may occur:

Jet Stream:

    1. Amplification and Slowing:
      • Climate change can lead to the amplification of atmospheric patterns, including the jet stream. This can result in larger north-south swings, which may contribute to more persistent weather conditions. Additionally, a warming Arctic relative to the mid-latitudes may slow down the jet stream.
    2. Stalled Weather Patterns:
      • A slower, more meandering jet stream can lead to the persistence of weather patterns, causing prolonged periods of extreme conditions such as heatwaves, cold spells, or heavy rainfall.
    3. Shifts in Track:
      • Climate change may alter the typical track of the jet stream, influencing where it tends to position itself. These shifts can impact regional weather patterns, including precipitation and temperature distributions.
    4. Increased Amplification:
      • As the Earth’s poles warm faster than the mid-latitudes, the temperature difference between the Arctic and lower latitudes decreases. This reduction in temperature gradient may lead to a more meandering and slower jet stream with larger north-south waves, a phenomenon known as “jet stream amplification.”
    5. Wavier Jet Stream:
      • The reduced temperature contrast between the Arctic and mid-latitudes can make the jet stream more susceptible to large, slow-moving waves. This wavier pattern can result in more persistent weather conditions, including prolonged periods of heatwaves, cold spells, droughts, or heavy rainfall.
    6. Increased Blocking Patterns:
      • A wavier and slower jet stream can lead to the formation of blocking patterns, where high or low-pressure systems persist in a particular location for an extended period. Blocking patterns can contribute to prolonged and extreme weather events.
    7. Slower Movement:
      • Some studies suggest that the jet stream is slowing down as a result of climate change. A slower jet stream can cause weather systems to move more slowly across the landscape, potentially intensifying the impacts of extreme events such as storms, heatwaves, or heavy rainfall.
    8. Changes in Zonal Flow:
      • The jet stream typically flows from west to east in a relatively straight line, a pattern known as zonal flow. Climate change may lead to more frequent disruptions of this zonal flow, causing the jet stream to meander and creating conditions for more extreme weather events.
    9. Impacts on Weather Extremes:
      • Changes in the jet stream can influence the occurrence and characteristics of weather extremes, including heatwaves, cold snaps, and intense storms. These changes can have significant implications for local and regional climate patterns.

    Atmospheric Rivers:

    1. Increased Moisture Content:
      • Warmer temperatures associated with climate change can enhance evaporation, increasing the moisture content of the atmosphere. This, in turn, can contribute to the development of more intense atmospheric rivers, which are channels of concentrated moisture in the atmosphere.
    2. Changes in Intensity and Frequency:
      • Climate change may lead to alterations in the intensity and frequency of atmospheric rivers. There is evidence suggesting that these phenomena could become more common and more potent, leading to heavier rainfall events and an increased risk of flooding.
    3. Altered Trajectories:
      • Changes in the jet stream’s position and behavior can influence the trajectories of atmospheric rivers. Variations in the jet stream can result in altered paths for these moisture-laden systems, affecting the regions that experience heavy rainfall and potential flooding.
    4. Extreme Weather Events:
      • Atmospheric rivers are often associated with extreme weather events, including heavy rainfall and flooding. Changes in the characteristics of atmospheric rivers due to climate change can contribute to an increased likelihood of severe weather events on the East Coast.

East Coast Atmospheric Rivers and AMOC (Atlantic Meridional Overturning Circulation) Brouse (2024)

Extreme Rainfall–surge Hazard Risk Basics and Atmospheric Rivers Brouse (2022)

West Coast Atmospheric Rivers Brouse (2023)

East Coast Atmospheric Rivers Brouse (2023)

Greenland Atmospheric Rivers Mukherjee (2023)

Owning a Shore Property and Flood Insurance

ALSO SEE:
The Reign of Violent Rain Brouse and Mukherjee (2023)
The Age of Loss and Damage Brouse (2023)
Climate Change Impacts on Flood Risks and Real Estate Values Sidd Mukherjee and Daniel Brouse (2023)

bookmark_borderTipping Cascades, Social-Ecological Systems, and the Hottest Year in History

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by Daniel Brouse
January 9, 2024

Human induced climate change is an exponential component of an unordered system (chaos theory). That means global warming is accelerating at a rapid rate in a complex way.

Unfortunately, even scientists are failing to see (let alone forecast) the rapid acceleration in climate change. Due to their complexity, the impacts of the Domino Effect are being underestimated. Tipping points are Critical Milestones that directly impact the rate of acceleration in climate change by multiplying the number and intensity of feedback loops. The Domino Effect is also known as “tipping cascades” in climate science. Cascading impacts in relation to tipping points include cascading impacts across biogeophysical and social systems. Until recently, scientist have been drastically underestimating the social-ecological systems. The University of Exeter reports, “There is a notable lack of topic clusters dedicated to how humans will be impacted by climate-related tipping cascades.”

The Age of Loss and Damage is a new way of thinking about economics by combining economics, climate science, statistics, and physics. Until now, economic models have been unfit to capture the full extent of climate damage. Traditionally, “integrated assessment models” (IAMs) were used to forecast “shock” events. IAMs use “quadratic function” to calculate GDP losses by squaring the temperature change, yet ignore other methods (such as the exponential function) that are better suited for rapid change. “Climate change is fundamentally different to other shocks because once it has hit, it doesn’t go away,” said Thierry Philipponnat, author of a report by Finance Watch, a Brussels-based public interest NGO on financial issues. “And if the fundamental assumption is flawed, all the rest makes little sense — if any.”

Reuters reported, “Critics say this (IAMs) choice is doomed to underplay the likely impact – particularly if the planet hits environmental tipping points in which damage is not only irreversible but happens at an ever-accelerating rate.” Thierry Philipponnat’s report, Finance in a Hot House World, concludes: “Climate risk is growing to disruptive levels throughout the financial system and the guardians of financial stability urgently need to adapt their tools to regain control.” The report calls for economic models that do not mislead, scenario analyses that prepare the market, and a new prudential tool to address the build-up of systemic climate risk.

Traditional economics is based upon the “costs and benefits” to society. Since there are no known long-term benefits of climate change to society, the Age of Loss and Damage economics focuses on the exponential costs of climate change to society.
— from The Age of Loss and Damage / Brouse (2023)

2023: The Hottest Year in Human History
2023 was a wake-up call to both biogeophysical and social-ecological scientists. The record breaking physical and economical impacts could be felt worldwide. The record warming year was seventeen times greater than any other record increase in history. Typically record breaking temperatures are measured in 100th degrees. There were also 200 consecutive days of record breaking temperatures. Typically there are one or two record breaking days in row. The increase in intensity and frequency of record breaking heat requires forecasting models to be recast.

2023 Biogeophysical Records

Global temperatures reached exceptionally high levels in 2023. The Copernicus Climate Change Service (C3S), implemented by the European Centre for Medium-Range Weather Forecasts on behalf of the European Commission with funding from the EU, monitored several key climate indicators throughout the year, reporting on record-breaking conditions such as the hottest month on record and daily global temperature averages briefly surpassing pre-industrial levels by more than 2°C. Unprecedented global temperatures from June onwards led 2023 to become the warmest year on record – overtaking by a large margin 2016, the previous warmest year.

Highlights: 

  • 2023 is confirmed as the warmest calendar year in global temperature data records going back to 1850
  • 2023 had a global average temperature of 14.98°C, 0.17°C higher than the previous highest annual value in 2016
  • 2023 was 0.60°C warmer than the 1991-2020 average and 1.48°C warmer than the 1850-1900 pre-industrial level
  • It is likely that a 12-month period ending in January or February 2024 will exceed 1.5°C above the pre-industrial level
  • 2023 marks the first time on record that every day within a year has exceeded 1°C above the 1850-1900 pre-industrial level. Close to 50% of days were more than 1.5°C warmer then the 1850-1900 level, and two days in November were, for the first time, more than 2°C warmer.
  • Annual average air temperatures were the warmest on record, or close to the warmest, over sizeable parts of all ocean basins and all continents except Australia
  • Each month from June to December in 2023 was warmer than the corresponding month in any previous year
  • July and August 2023 were the warmest two months on record. Boreal summer (June-August) was also the warmest season on record
  • September 2023 was the month with a temperature deviation above the 1991–2020 average larger than any month in the ERA5 dataset
  • December 2023 was the warmest December on record globally, with an average temperature of 13.51°C, 0.85°C above the 1991-2020 average and 1.78°C above the 1850-1900 level for the month. You can access information specific for December 2023 in our monthly bulletin
  • Global average sea surface temperatures (SSTs) remained persistently and unusually high, reaching record levels for the time of year from April through December
  • 2023 saw a transition to El Niño. In spring 2023, La Niña came to an end and El Niño conditions began to develop, with the WMO declaring the onset of El Niño in early July.
  • High SSTs in most ocean basins, and in particular in the North Atlantic, played an important role in the record-breaking global SSTs
  • The unprecedented SSTs were associated with marine heatwaves around the globe, including in parts of the Mediterranean, Gulf of Mexico and the Caribbean, Indian Ocean and North Pacific, and much of the North Atlantic
  • 2023 was remarkable for Antarctic sea ice: it reached record low extents for the corresponding time of the year in 8 months. Both the daily and monthly extents reached all-time minima in February 2023
  • Arctic sea ice extent at its annual peak in March ranked amongst the four lowest for the time of the year in the satellite record. The annual minimum in September was the sixth-lowest
  • The atmospheric concentrations of carbon dioxide and methane continued to increase and reached record levels in 2023, reaching 419 ppm and 1902 ppb respectively. Carbon dioxide concentrations in 2023 were 2.4 ppm higher than in 2022 and methane concentrations increased by 11 ppb.
  • A large number of extreme events were recorded across the globe, including heatwaves, floods, droughts and wildfires. Estimated global wildfire carbon emissions in 2023 increased by 30% with respect to 2022 driven largely by persistent wildfires in Canada

2023 Social-Ecological Records

NOAA: 2023 A historic year of U.S. billion-dollar weather and climate disasters

In 2023, the U.S. experienced 28 separate weather and climate disasters costing at least 1 billion dollars. That number puts 2023 into first place for the highest number of billion-dollar disasters in a calendar year and included:

  • 1 winter storm/cold wave event (across the northeast U.S. in early-February).
  • 1 wildfire event (firestorm destroying town of Lahaina on Maui Island of Hawaii).
  • 1 drought and heat wave event (focused across the central and southern U.S.).
  • 4 flooding events (in California, Florida, and across the eastern and northeastern U.S.).
  • 2 tornado outbreaks (across the central and eastern U.S.).
  • 2 tropical cyclones (Idalia in Florida and Typhoon Mawar in Guam).
  • 17 severe weather/hail events (across many parts of the country).

2023 was also deadly, causing at least 492 direct or indirect fatalities — the 8th most disaster-related fatalities for the contiguous U.S. since 1980.

What Can I Do?
There are plenty of things you can do to help save the planet. Stop using fossil fuels. Consume less. Love more. Here is a list of additional actions you can take.

ALSO SEE: Climate Change: Rate of Acceleration / Brouse and Mukherjee (2023)

The Human Induced Climate Change Experiment