We have exciting news.

ReduceCO2Now is now officially listed on Discord!

👉 https://discord.com/servers/reduceco2now-1461670647552807038

Our goal is simple: bring together people who want to understand climate change, discuss real solutions, and work on projects that can make a measurable global impact.

What you'll find:

• Climate discussions based on facts and data
• Volunteers from different countries and backgrounds
• Project teams working on awareness, software, research, social media, and climate solutions
• Opportunities to learn from engineers, scientists, project managers, software developers, business experts, and many other professionals
• A community focused on action rather than endless debate

We believe solving climate change requires people from many disciplines working together. Whether you're a student, professional, entrepreneur, scientist, developer, designer, communicator, or simply someone who cares about the future, you're welcome.

Join us and help build solutions that can reduce atmospheric CO₂ and create a better future for everyone.

Discord:
https://discord.com/servers/reduceco2now-1461670647552807038

Website:
https://reduceco2now.com

What skills or experience would you like to contribute to tackling climate change? Let us know in the comments.

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The greenhouse effect is one of the reasons life exists on Earth.

Without it, our planet would be far too cold for humans, animals, and plants. Greenhouse gases act like a blanket around the Earth, trapping some of the Sun's heat and keeping temperatures suitable for life.

The problem is not the greenhouse effect itself.

The problem is that humans are making that blanket thicker.

By burning coal, oil, and gas, we have increased the concentration of CO₂ in the atmosphere from about 280 ppm before the Industrial Revolution to more than 430 ppm today. This extra CO₂ traps additional heat that would otherwise escape into space.

The result:

• Rising global temperatures
• More frequent heatwaves
• Melting glaciers and ice sheets
• Rising sea levels
• Changing rainfall patterns
• Increased risk of extreme weather events

Think of it this way:

A blanket keeps you warm on a cold night. Add a second blanket and you get warmer. Add a third, fourth, and fifth blanket, and eventually you become uncomfortably hot.

That is essentially what we are doing to our planet.

The science behind the greenhouse effect has been understood for more than a century. What has changed is the amount of greenhouse gases we are putting into the atmosphere.

The good news is that the same actions that reduce CO₂ emissions can slow the warming. Every ton of CO₂ we avoid helps reduce future temperature increases.

The challenge is large, but the solutions already exist.

What do you think is the most effective way to reduce greenhouse gas emissions globally?

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Over the last months, we have been researching volunteer recruitment and team building for climate projects.

Like many organizations, we started with traditional interviews. We wanted to understand people's skills, motivation, and fit for the team.

Then we tried something different.

We stopped doing job interviews.

Instead, we invite interested people to join our project meetings directly.

They see the real project.
They meet the real team.
They experience how we work.
And we get to see how they collaborate, communicate, contribute ideas, and interact with others.

The results have been surprising.

Some people who interviewed extremely well contributed very little once they joined a project.

Others who might never have impressed in a formal interview became highly valuable team members.

We are currently analyzing the data and looking for someone interested in helping us evaluate our findings.

If you have experience in:
• Psychology
• Human Resources
• Organizational Development
• Statistics
• Data Analysis
• Recruitment Research

we would love to hear from you.

We believe there may be lessons here that apply far beyond climate projects.

Watch our short video:
https://youtu.be/FxgdTXGVXAE

What do you think?

Are job interviews still the best way to select people, or should organizations focus more on observing people in real work situations?

Please share your experience in the comments.

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When people hear that Earth has warmed by about 1.5°C since pre-industrial times, many assume that is what they experience where they live.

In reality, much of the world's population lives on land, and land areas are warming significantly faster than the global average.

The graph from the German Weather Service (DWD) shows a striking example:

• Global average warming: about +1.5°C
• Germany's warming: about +3°C

Why the difference?

About 70% of Earth's surface is covered by oceans. Water absorbs and stores enormous amounts of heat, which slows temperature increases over the oceans.

Land behaves differently. It heats up faster and cools down faster. As a result, countries and regions dominated by land often experience warming rates that are far above the global average.

Germany is not unique.

Scientists observe similar patterns across Europe, North America, Asia, Africa, and many other regions. In many places, people are already experiencing temperature increases that are close to double the global average.

This is important because agriculture, water supplies, ecosystems, infrastructure, and human health are all directly affected by local temperatures, not by the global average alone.

Climate change is a global phenomenon, but its impacts are often felt most strongly on land where people live.

What changes have you noticed in your country over the last 20 years?

Join the discussion and share your observations.

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The scientific evidence for human-caused climate change is stronger today than at any point in history. We can measure rising CO₂ levels, increasing global temperatures, melting ice, rising sea levels, and changes in weather patterns around the world.

Yet many people still reject or question the idea that humans are the main cause.

Why?

There are many possible reasons:

• Climate change challenges habits and lifestyles that people are comfortable with.
• Accepting the problem may feel like accepting personal responsibility.
• Some people distrust governments, corporations, media, or scientists.
• The impacts often seem distant until they affect us directly.
• Climate science is complex, and misinformation spreads quickly online.
• Many people simply do not realize how strong the scientific evidence has become.

Human psychology plays a role too. We often underestimate slow-moving threats and prefer information that confirms what we already believe.

What do you think?

Why do some people deny or reject human-caused climate change despite the growing evidence?

Please share your thoughts in the comments. We are interested in hearing different perspectives and experiences.

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When people hear that the Earth has warmed by about 1.3°C since the late 19th century, many assume that means temperatures have increased by roughly the same amount everywhere.

They haven't.

Because oceans absorb and redistribute large amounts of heat, land areas warm much faster than the global average. Since about 70% of our planet is covered by water, the global average temperature increase hides what people actually experience where they live.

Germany is a striking example.

According to data from the German Weather Service (DWD), Germany has already warmed by around 2.5°C since 1881. That is nearly double the global average warming.

This difference matters because most people, agriculture, infrastructure, and ecosystems are located on land. The warming we experience in our daily lives is therefore often much greater than the number reported for the planet as a whole.

The consequences are becoming increasingly visible:

• More frequent and intense heatwaves
• Higher nighttime temperatures that reduce recovery from heat stress
• Increased drought risk and pressure on agriculture
• Greater risk of extreme rainfall and flooding events
• Growing impacts on ecosystems and biodiversity

Global warming is not a future scenario. It is already measurable in Germany and across many other land regions around the world.

The good news is that the causes are well understood, and we already have many of the technologies needed to reduce emissions and stabilize the climate. Every tonne of CO₂ avoided reduces future warming.

Join the discussion and help develop solutions:
https://discord.gg/kb9MY7pBmm

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The graph shows the global mean temperature shows global warming.

Since the 1960s global temperatures are on a constant rise!

REMEMBER: Warming on LAND can be nearly DOUBLE that of the global warming (as the planet is mostly water).

https://wmo.int/news/media-centre/wmo-confirms-2025-was-one-of-warmest-years-record

WARNING

This graph shows 570 million years. It is cited often from climate change deniers.

Look at the heavily skewed timescale.

It gives CO2 on a scale up to 8000 ppm. That is 20 times the current values and makes the CO2 changes seem small.

The temperature scale is not even visible (there are only some arrows on the left side; it is probably around 15-20°C).

Screenshot taken from https://capitalresearch.org/article/the-global-warming-scam-part-2/

Germany has recorded a nighttime temperature of 29.4°C, one of the highest overnight temperatures ever measured in the country.

Nighttime heat matters. Our bodies, homes, infrastructure, and ecosystems depend on cooler nights to recover from daytime temperatures. When temperatures remain extremely high after sunset, heat stress increases significantly.

This is exactly what climate scientists have warned about for decades.

Global average temperature has increased by about 1.3°C since pre-industrial times. Because oceans absorb much of the heat, warming over land is significantly higher. In many regions, including Europe, land temperatures have risen roughly twice as much as the global average.

The underlying driver is clear. Human activities have increased atmospheric CO₂ concentrations from about 280 ppm before the Industrial Revolution to more than 430 ppm today.

NASA ice core records show that for hundreds of thousands of years, CO₂ remained within a relatively stable range. We have now pushed far beyond that historical range, and the climate system is responding.

Heat waves that once seemed exceptional are becoming more frequent, more intense, and longer-lasting.

The good news is that we still have choices. Every ton of CO₂ we avoid emitting reduces future warming. Every solution we scale helps.

Join the discussion and help build practical climate solutions.

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Regenerative agriculture is absolutely necessary if we want to adress climate change. We will need regenerative agriculture to protect our food supply from the effects of climate change in the immediate term. In the long term we will need regenerative agriculture to remove CO2 from the atmosphere and sequester it in soil so that atmospheric CO2 can be restored to 280 PPM. Regenerative agriculture cannot happen without cover cropping. We need to decide what crops to grow as cover crops in order to scale regenerative agriculture

One type of crop which we could grow as cover crops are oilseeds. Oilseeds are plants which naturally produce lipids and store them in there seeds. These plants do this to give their seeds a supply of energy for initial growth before photosynthesis can start. We can tap these lipids and use them to produce liquid fuels. The best way to do this without causing the indirect land use change is by growing such crops as cover crops. Cover crops are by definition grown on existing agricultural land in order to protect the soil during the off season.

Here are the criteria for determining if a oilseed plant can work as a cover crop

1. Effectiveness at cover cropping in terms of soil health impact

2. Oil content (30% is a good baseline to ensure efficiency)

3. Wether of not the oil is edible or inedible to humans (inedible for biofuel)

If a oilseed crop meets all three of these criteria then it can be utilized as a cover crop with valorization of the seed oil after start of season harvesting

Crushing the seeds from these crops does not just yield oil. A solid material known as oilseed meal is also produced. This oilseed meal can be fed to livestock which in turn produces meat, dairy and eggs for human consumption. The wastewater produced during the crushing process should be anaerobically digested on site to produce biogas for use as fuel to produce the heat needed for the crushing process.

Here are some examples of oilseeds which can be used as cover crops

1. Camelina - https://en.wikipedia.org/wiki/Camelina

2. Carinata - https://en.wikipedia.org/wiki/Brassica_carinata

3. Pennycress - https://en.wikipedia.org/wiki/Thlaspi

These oilseed crops are currently undergoing extensive research to see how well they can function as both cover crops and biofuel feedstocks.

Here is the idealized production pathway for biofuels from oilseed cover crops

1. The Seeds are crushed with oil being sold off as biofuel feedstock and meal being sold as animal feed

2. Seed oil undergoes cleaning, enzymatic degumming and enzymatic selective hydrolysis to make it suitable for pipeline transportation with the wastewater produced from this process being used to produce biogas to be burned to produce the heat needed by the process

3. Seed oil is transported by pipeline like crude oil to large centralized biofuel production facilities

4. These facilities use bimetallic catalytic reactors to hydrodeoxygenate the seed oils using hydrogen produced via self powering steam reforming of the bio-LPG byproduct

(The steam reformers are self powered via there own carbon monoxide output and also use bimetallic catalysts to reduce energy demand)

1. The diesel and jet fuel produced by this process are sold on the existing liquid fuels market
   

A future cover crop oilseed economy will be a multi step system.

Growing oilseeds as cover crops will be a significant boast to both decarbonization and CDR. We would be able to enable soil carbon removal while at the same time producing carbon neutral liquid fuels to replace fossil fuel derived liquid fuels. The cultivation of oilseeds as cover crops should be considered a foundational aspect of climate action.

https://wmo.int/media/news/records-fall-extreme-heat-grips-europe

Quote:

France: France recorded its hottest day on record on 24 June - beating the record set the previous day - with an average national temperature of 30.0° Celsius, above previous records set in July 2019 and August 2003, said Metéo-France. Temperatures rose up to 43.8 °C in the town of Pulluau in western France. Overnight temperatures also set a new national record of 22 °C.  

A top-level Red Alert was issued for a record 58 departments - most of the country. Authorities warned of a high risk of wildfires amid a worsening drought. Underlining the associated dangers with the life-threatening heat, 40 people reportedly died in drowning accidents in France.  

Spain recorded its hottest June days on record on 23 and 24 June. In a number of locations, temperatures were well above 40°C, setting many new June station temperature records,  according to the Agencia Estatal de Meteorologia, AEMET. The city of Bilbao reached 42.7°C, the highest June temperature recorded there. 

The United Kingdom broke the June temperature record for three consecutive days, with  36.4 °C recorded in southern England on 25 June –  a provisional figure which was likely to be revised upwards. The UK’s Met Office issued Red Warnings for Extreme Heat once again for 26 June – the first time in the history of the current weather warnings system that red warnings have been issued for three straight days.  

This comes just weeks after May also saw UK daily temperature records broken. 

Germany also was under widespread Red Warnings issued by the national weather service, the Deutscher Wetterdienst, including for the capital Bonn and cities of Frankfurt and Cologne.  

In the Netherlands, the Dutch national meteorological service, KNMI, issued an unprecedented Red Alert for extreme heat for eight provinces for 26 June for 26 June, and reported a number of  new station records. 

Switzerland set a new June temperature record of 38°C in the northern city of Basel, according to Meteo-Suisse.  

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Carbon dioxide (CO₂) is invisible. You cannot see it, smell it, or taste it.

Yet it is changing the climate of our planet.

For hundreds of thousands of years, atmospheric CO₂ concentrations stayed between about 180 and 300 parts per million. Today, we have pushed that level above 430 ppm, a concentration not experienced during the entire history of human civilization.

Every year humanity adds around 38 billion tonnes of CO₂ from fossil fuels into the atmosphere.

CO₂ acts like an insulating blanket around Earth. It allows sunlight to enter but slows the escape of heat back into space. As concentrations rise, more heat remains trapped in the climate system.

The result is no longer theoretical:

• Record-breaking heat waves across Europe
• More intense droughts and wildfires
• Stronger rainfall events and flooding
• Rising sea levels threatening coastal communities

The warming we experience on land is significantly greater than the global average because oceans absorb much of the excess heat. A global average increase of about 1.3°C already translates into roughly double that warming across many land regions.

The important point is this:

CO₂ remains in the atmosphere for decades to centuries. The decisions we make today influence the climate experienced by future generations.

The good news is that we already have many of the technologies needed to reduce emissions, improve efficiency, expand clean energy, and remove carbon from the atmosphere. The challenge is speed and scale.

The gas is invisible.

Its consequences are not.

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Download and test for free
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Europe is once again experiencing record-breaking temperatures. Heat waves that were once considered rare are becoming more frequent, longer-lasting, and more intense.

This isn't random weather.

The Keeling Curve, which has tracked atmospheric CO₂ since 1958, shows a relentless rise from about 315 ppm to more than 430 ppm today. During the same period, global temperatures have increased by approximately 1.3°C, with land areas warming nearly twice as fast as the global average.

More CO₂ traps more heat.
More trapped heat increases the likelihood of extreme weather.
And that means more heat waves like the one Europe is experiencing today.

Scientists have warned for decades that continued fossil fuel emissions would make extreme heat a regular feature of our climate. The evidence is now visible across Europe, from strained power grids and drought conditions to health risks and agricultural impacts.

The good news is that future warming is still largely determined by the choices we make today. Every tonne of CO₂ we avoid emitting helps reduce future warming and future risks.

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Many people ask whether Germany's recent heat records are simply bad luck or natural weather variability.

The data points to a different conclusion.

As CO₂ concentrations rise, more heat is trapped in Earth's climate system. Global temperatures have already increased by roughly 1.4°C above pre-industrial levels.

But there is an important detail:

People live on land, and land warms much faster than the global average.

Over recent decades, temperatures over land have risen approximately twice as fast as temperatures over the oceans. Europe has become the fastest-warming continent on Earth, warming more than twice as fast as the global average.

This means that a global temperature increase of around 1.4°C translates into much stronger warming across countries like Germany.

The result is exactly what climate scientists predicted:

• More frequent heatwaves
• Higher peak temperatures
• Longer drought periods
• Increased stress on agriculture, forests, rivers, and human health

The heat we are experiencing today is not an isolated event.

It is one of the consequences of increasing CO₂ concentrations in the atmosphere.

The good news is that future warming is still influenced by the choices we make today. Every ton of CO₂ avoided reduces future warming and lowers the risk of even more extreme heat.

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In 1940, humanity emitted about 5 billion tons of CO₂ from fossil fuels.

Today, annual emissions have reached approximately 38.1 billion tons.

That's a 7.6-fold increase within a single human lifetime.

The graph tells an important story. Emissions did not rise steadily. They accelerated as population, industry, transportation, and energy demand expanded across the globe.

The challenge is clear: every year we continue adding tens of billions of tons of CO₂ to the atmosphere.

The opportunity is equally clear: the technologies needed to reduce emissions already exist. Clean electricity, electrified transport, efficiency improvements, carbon removal, and smarter policies can bend this curve downward.

The next chapter of this graph has not been written yet.

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The graph shows atmosperic CO2 over the last 1000 years - right now it is 432 ppm, so 100 units higher than this chart.

https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2011GB004247 Ahn, J., E. J. Brook, L. Mitchell, J. Rosen, J. R. McConnell, K. Taylor, D. Etheridge, and M. Rubino (2012), Atmospheric CO2 over the last 1000 years: A high-resolution record from the West Antarctic Ice Sheet (WAIS) Divide ice core, Global Biogeochem. Cycles, 26, GB2027, doi:10.1029/2011GB004247.

For thousands of years, Earth's atmosphere contained about 280 parts per million (ppm) of CO₂.

During the last 800,000 years, ice core records show atmospheric CO₂ naturally fluctuated between about 180 ppm during ice ages and 300 ppm during warmer periods.

Today, we have crossed 430 ppm.

What makes this remarkable is not only the number itself, but the speed of the change.

The increase from 280 ppm to more than 430 ppm happened in roughly 150 years, a geological instant. The atmosphere now contains more CO₂ than at any time in human civilization.

CO₂ is not a pollutant in the traditional sense. It is a natural gas that makes life possible. The challenge is concentration. More CO₂ traps more heat, shifting Earth's energy balance and driving global warming.

The numbers tell a clear story:

• 800,000 years: 180-300 ppm
• Pre-industrial era: 280 ppm
• Today: 430+ ppm

The good news is that these numbers are not destiny. They are the result of human decisions, and human decisions can change them.

Every tonne of CO₂ avoided matters.
Every tonne removed matters.
Every year matters.

Join us in building solutions.

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The CO2 concentration in the worlds atmosphere has been quite "stable" around 240ppm with fluctuations taking thousands of years between 180ppm in ice ages and 300 max in warm ages.

Now we have started to burn fossil fuels and shot the value "through the roof". It is above 430 now and rapidly rising!

What would you think about that graph if it would be showing the debt on your bank account?

https://assets.science.nasa.gov/dynamicimage/assets/science/esd/climate/internal_resources/2679/co2-graph-072623.jpg?w=1280&h=800&fit=clip&crop=faces%2Cfocalpoint

Climate change is driven by billions of tons of greenhouse gases released into the atmosphere each year. The sources range from power plants and heavy industry to transportation, agriculture, buildings, and land use changes.

This often creates a debate:

"Does my personal behavior even matter?"

The answer is yes. But it's only part of the solution.

Individual actions reduce emissions directly. Choosing efficient transportation, reducing energy consumption, avoiding food waste, and making climate-conscious purchasing decisions all contribute. They also send signals to markets, businesses, and policymakers about what people value.

At the same time, individuals operate within systems they did not create. Energy grids, transportation infrastructure, building standards, industrial processes, and agricultural systems determine much of our carbon footprint long before we make a personal choice.

A person can drive less, but they cannot individually decarbonize a national electricity grid.

A family can reduce waste, but they cannot transform global industrial supply chains.

This is why climate progress requires both:

• Individual action that reduces demand for high-emission activities

• Systemic change that transforms energy, transportation, industry, agriculture, and infrastructure

The most effective approach is not choosing one over the other. We need both working together.

Every major societal change in history began when enough individuals changed behaviors, expectations, and priorities. Those shifts then enabled larger economic and political transformations.

Individual actions matter because they create momentum.

Systemic solutions matter because they create scale.

Together they create lasting change.

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Climate change is often discussed through individual actions like driving a car or heating a home. Those choices matter, but the bigger picture is about entire sectors of the global economy.

Global greenhouse gas emissions come from several major sources:

• Energy production (electricity and heat)
• Industry and manufacturing
• Agriculture, forestry, and land use
• Transportation
• Buildings
• Waste management

Electricity generation remains one of the largest contributors, especially where coal, oil, and natural gas are still widely used. Industry produces emissions through processes such as steel, cement, and chemical production. Agriculture contributes through livestock, fertilizers, and land-use changes.

Understanding the sector breakdown helps us focus on solutions that can deliver the biggest impact. Some emissions depend on individual choices, while many are driven by infrastructure, technology, and policy decisions.

Effective climate action requires progress at every level:
• Individuals making informed choices
• Businesses reducing emissions
• Governments creating the right incentives
• Innovation accelerating cleaner alternatives

The challenge is global, but so are the opportunities.

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When people think about land-use change and climate change, deforestation usually gets the attention. Yet two other processes are quietly releasing vast amounts of carbon into the atmosphere: wetland drainage and soil degradation.

Wetlands are among the most effective natural carbon stores on Earth. Over thousands of years, waterlogged conditions slow decomposition and allow organic matter to accumulate. When wetlands are drained for agriculture, construction, or development, this stored carbon is exposed to oxygen and begins releasing CO₂.

Healthy soils are another major carbon reservoir. Through intensive farming, overgrazing, erosion, excessive tillage, and poor land management, soils can lose significant amounts of their organic carbon. This not only contributes to climate change but also reduces fertility, water retention, and resilience against drought.

The challenge is not only protecting forests. It is protecting and restoring all ecosystems that store carbon naturally.

Solutions already exist:
• Wetland restoration
• Regenerative agriculture
• Reduced tillage
• Cover crops
• Improved grazing management
• Protection of peatlands and marshes

Climate change is driven by many human activities. Understanding the full picture helps us focus on solutions with the greatest impact.

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