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Historical Climate Trends: How Has Climate Changed in the Past

how has climate changed in the past

As we delve into the rich tapestry of Earth’s climatic history, it becomes evident that historical climate shifts have long shaped our planet’s environment. From the lull of glacial periods to the peak of interglacials, the Earth has experienced climatic shifts over time that tell a story of natural evolution and the increasingly evident impact of human influence. In recent centuries, however, these changing climate patterns have begun to accelerate at an alarming rate, diverging from past climate variations previously seen in the geological record.

By examining factors such as global average surface temperature increases and the intensification of weather phenomena, we gain insight into how the Earth’s climate system is responding to a significantly higher concentration of atmospheric greenhouse gases. The nuanced understanding of these shifts is crucial for forecasting future climatic conditions and developing strategies to mitigate the impact of these transformations.

Key Takeaways

  • Around 2-degree Fahrenheit rise in temperature since the pre-industrial era has major climatic consequences.
  • Land areas, particularly the Arctic, are warming significantly faster than ocean regions.
  • Global average temperature measurements inform us about changes in Earth’s energy budget over time.
  • 2023 marked every month as among the seven warmest for that respective month, with new records in late-year temperatures.
  • Human activities have been a central cause of the rapid increase in greenhouse gases, leading to observable climatic shifts.

Understanding Earth’s Climatic History

Delving into the evolution of past climates offers a window into the dynamics that have governed Earth’s environment through the ages. The study of past climate variations provides a narrative of ancient climate change, aiding our comprehension of present and future trends. Recognizing the crucial role of Earth’s climatic history is essential in making sense of recent meteorological phenomena and their amplified intensity.

Scientists, in their quest to unravel the complexities of climatic progression, have established the concept of a global average temperature—a convenient tool to assess shifts in the planet’s energy budget. This collective measure involves an intricate dance of numerical interpretation, where temperature anomalies (the variance between actual temperature readings and established long-term averages) narrate the ongoing tale of Earth’s thermal blueprint.

The latest Global Climate Report from NOAA presents an undeniable upward surge in Earth’s surface temperature. Independent researchers worldwide corroborate this trend, weaving a consensus that emphasizes a pronounced warming pattern unprecedented in recent history. Such global collaboration has fortified the methodologies for tracking climatic changes, offering more than anecdotal evidence but rather a statistically sound testament to our transforming world.

Beyond the intricate measurements and algorithms lie the tangible implications that reverberate across continents and oceans—a narrative of climatic shifts propelled not only by natural forces but also by the unwavering influence of anthropogenic activities.

  • A consistently rising global surface temperature underscores the urgency for a deeper understanding of climatic dynamics.
  • Temperature anomaly datasets serve as climatic storylines, unveiling trends that signpost both past and emergent weather phenomena.
  • The global average temperature transcends mere metrics, reflecting humanity’s indelible footprints across the fabric of our planetary climate.

In this way, the study of Earth’s thermal past offers not just historic insight but also a proxy for anticipation. It stakes a claim for foresight over happenstance, empowering society with knowledge—knowledge to navigate, to adapt, and to innovate for the sake of tomorrow’s climate.

How Has Climate Changed in the Past

The examination of changing climate patterns reveals a clear upward trend, signaling a shift toward global warming that is predominantly a consequence of human impact. Historical climate shifts, such as the transition from the Little Ice Age to current conditions, have typically been gradual. However, the rate of change has markedly increased due to emissions of greenhouse gases.

Scientific consensus, as established by the Intergovernmental Panel on Climate Change (IPCC), supports the view that the recent warming trend is pronounced, asserting it as unequivocal and chiefly driven by human activity. Data highlight the warming of our planet’s surface, aligning with the discernible increase in the production of well-mixed greenhouse gases alongside other human-powered drivers of climate change. Naturally occurring factors, such as solar radiation and volcanic activity, play a role but are substantially overshadowed by anthropogenic influences.

Climate Driver Impact on Global Temperatures (1850-1900 to Present) Warming Influence Cooling Influence
Well-Mixed Greenhouse Gases Significant High Low
Other Human Drivers (e.g., aerosols) Moderate Varied Varied
Natural Drivers (solar, volcanic) Minimal Minimal Minimal
Internal Variability Variable Low Low

It’s important to recognize these factors not as isolated incidents but as components of an interconnected system affecting historical climate shifts. Our understanding of these trends is amplified through the study of climate proxies such as ice cores, tree rings, and sediment layers, which serve as historical records of past climatic conditions.

  • The role of human activities in global temperature rise is now seen as a primary driver of recent climatic change.
  • Concentrations of carbon dioxide and other greenhouse gases have increased sharply, resulting in the amplification of the greenhouse effect.
  • Climatological studies attribute the bulk of the recent temperature rise to anthropogenic causes rather than natural variability.

Changing climate patterns data visualized

The data presented above is not simply a cause for academic curiosity but represents a clarion call for action. It underscores the paramount importance of addressing the root causes of changing climate patterns to mitigate the impacts of future historical climate shifts.

Ancient Climate Shifts and Their Causes

Peering into the depths of Earth’s climatic archives reveals a pattern of ancient climate change pivotal in sculpting today’s planetary landscape. These ancient changes offer crucial context for understanding current climatic anomalies.

The Ice Age Cycles and Solar Variations

The natural oscillation between ice age cycles and warmer interglacial periods marks Earth’s history with a rhythm dictated by orbital shifts. These cyclical changes, substantial in their global impact, are the results of minute variances in Earth’s orbit and axial tilt. These astronomical variations adjust the amount and distribution of solar energy received by our planet, a phenomenon known as Milankovitch cycles. The evidence of these cycles is imprinted in geological records, telling a tale of a ceaselessly dynamic Earth.

Volcanic Activity and Its Impact on the Climate

The powerful forces beneath Earth’s crust manifest above as volcanic activity climate impact, another natural architect of climate. Volcanic eruptions have historically ejected massive quantities of ash and gases into the atmosphere, creating aerosols that reflect solar radiation and induce temporary cooling. The climate response to such events extends beyond immediate, dramatic temperature drops, influencing longer-term climatic shifts and affecting global circulation patterns.

ancient climate change and volcanic activity impact

A closer look at the intricate details of these ancient climatic influencers deepens our appreciation of their power and reminds us of their timeless role in Earth’s ever-changing climate story.

  • The ice age cycles have been a repeating pulse of change throughout planetary history, mirrored by shifts in flora and fauna.
  • Volcanic activity has the capacity to shroud the planet’s atmosphere, altering climate patterns and affecting life on Earth.

The uncovering of these ancient climatic mechanisms imploringly reflects on the stark contrast between the natural course of Earth’s climatic evolution and the rapid alterations introduced by human activities.

Global Warming: The Modern Climate Anomaly

Modern climate change has ushered in an era of global environmental transformation that is distinct from any prior climate variation in Earth’s history. A significant factor distinguishing modern climate change from historical shifts is its primary cause: human activities that have escalated since the mid-1800s, leading to the proliferation of greenhouse gas emissions. The accumulation of these gases in the atmosphere has effectively altered its composition, fostering a blanket that traps more of the Sun’s energy and yields a gradual but unwavering uptick in the average global temperature.

The pace at which this global warming is occurring has confounded scientists, who note that the rate of increase in global temperatures is without precedent in many recent millennia. This swiftness is most poignantly reflected in the drastic shifts in climate data over the years, with a seemingly incessant march toward warmer conditions.

The following table highlights the profound changes in global temperature and their relation to human activity, providing a clear contrast between the natural and current anthropogenic drivers of climate change:

Year Global Temperature Anomaly (°F) Carbon Dioxide Levels (ppm) Attributed Cause
Pre-Industrial Era 0 Approx. 280 Natural Variability
Mid-1800s Begin Increase Begin Rise Onset of Industrialization
Late 20th Century Marked Uptick 350+ Accelerated Industrial Activity
21st Century Continued Rise 400+ Industrial Activity, Deforestation

This chart clearly demonstrates how the increase in global warming correlates with the rise in greenhouse gas concentrations, a signal of modern climate change resulting largely from anthropogenic causes.

Modern climate change data showing global warming trend

  • The increase in Earth’s average temperature is synchronously matched by the growth in levels of carbon dioxide, solidifying the relationship between human activity and modern climate change.
  • The transition from the pre-industrial natural climate cycle to our current, abnormal warming trend marks a significant divide in our planet’s climatic history.
  • The ongoing trends suggest that without substantial mitigation efforts, we can expect the anomalies witnessed today to become increasingly severe and irreversible.

The phenomenon of global warming as it stands is not just a scientific concern, but a harbinger of the need for environmentally transformative action that resonates on a global scale. The narrative of Earth’s changing climate continues, with modern developments writing new chapters at a rate that calls for both acknowledgment and responsive, sustainable strategies.

The Significance of a 2-Degree Increase in Global Temperatures

The seemingly modest figure of a 2-degree increase in global temperatures harbors substantial consequences for the Earth’s climate. This slight uptick in the mercury belies a spectrum of profound environmental transformations that paint a concerning picture for the near future. Recognizing the significance of this threshold is pivotal when considering the far-reaching effects on our planet’s weather, ecosystems, and polar regions.

Changes in Weather Patterns

With a 2-degree Fahrenheit rise, the planet has seen alarming weather pattern changes. Recent trends show an intensification of extreme weather events—ranging from severe droughts to cataclysmic hurricanes. The frequency of heavy rainfall events has surged, arming storms with more water and increasing the potential for flooding and infrastructure damage. These aren’t mere changes, but signals of a new, volatile era of weather.

Impact on Sea Ice and Polar Regions

The polar regions impact is nowhere more apparent than in the precipitous sea ice decrease. The Arctic in particular has endured a rapid decline in sea ice extent, exacerbating global sea-level rise and imperiling unique marine habitats. The loss of ice also accelerates warming further through a process known as the albedo effect, wherein less ice means less sunlight is reflected back into space.

Effects on Biodiversity and Ecosystems

The biodiversity effects of a 2-degree warming are manifold and deeply disconcerting. Ecosystems, both terrestrial and marine, are experiencing a significant shift, as species struggle to adapt to the spiking temperatures. For some, this means migration to cooler climes, while others face the risk of extinction. These disruptions in biodiversity portend a ripple effect that threatens food security, human health, and the delicate balance of the world’s biomes.

  • Rising temperatures leading to more intense and frequent weather extremes
  • Melting polar ice contributing to higher sea levels
  • Shifting ecosystems and the challenge to biodiversity sustainability

Climatic Shifts Over Time: From the Pre-Industrial Era to Today

The narrative of Earth’s climate encompasses a time spectrum that extends well beyond the advent of industrial society, touching upon eras when human activity played a negligible role in shaping the environment. The comparison between our pre-industrial climate and the current atmospheric conditions lays bare the climatic shifts over time, dramatized by the marked escalation of greenhouse gas concentrations in the atmosphere.

Historical data conjures an image of a world that operated within the bounds of natural variability, while contemporary figures present a starkly different reality. The magnitude of change, especially in terms of global average temperatures, signals an accelerating departure from the relatively stable pre-industrial climate.

According to NOAA’s 2023 Global Climate Report, a substantial increase in Earth’s temperature reflects a significant change in accumulated heat—ushering in extremes of weather, transformations in habitats, and challenges for global biodiversity.

Let us consider the facts: A mere 2-degree Fahrenheit (approx. 1-degree Celsius) rise since the pre-industrial era denotes a substantial influx of energy, affecting the planet’s climatic machinery. The primary suspects behind this warming trend are anthropogenic emissions, which constitute a formidable force of change dominating over natural climatic influencers such as solar radiation and volcanic activity. The table below outlines the profound impact of this temperature increase:

Aspect Pre-Industrial Climate Current Observations
Global Average Surface Temperature Increase Baseline ~2°F (1°C)
Rate of Temperature Increase Natural Variability Accelerated Trend
Concentration of Atmospheric Greenhouse Gases ~280 ppm CO2 400+ ppm CO2
Climate Extremes and Variability Seasonal and Regional Differences Intensifying Extremes Globally

The steady increase reflected in global temperature recordings is striking, illuminating the urgent need to understand and address the contributors to these climatic shifts over time. The pre-industrial climate comparison serves not solely as a benchmark but also as a somber reminiscence of lost climate stability.

NOAA’s insights further compel us to acknowledge the rate of change we’re witnessing: a climate quickly departing from the familiar rhythms of Earth’s historical narrative. This unpredictability symbolizes the new climate reality, wherein each consecutive year writes a story of extreme weather, eroding icescapes, and ecological upheaval—a relentless march toward an unknown climatological frontier.

Climatic shifts over time visual chart

As we stand at this pivotal crossroads, the evidence beckons us to steer humanity towards a concerted response—one that is informed, proactive, and unyielding in the face of climatic adversity. With strategic action and global collaboration, we may yet slow the tempest of change and reclaim a measure of stewardship over our planet’s climate destiny.

The Human Factor: Greenhouse Gas Emissions and Climate Change

Since the dawn of the industrial revolution, human activities have initiated significant environmental changes, notably the increase in greenhouse gas emissions, which are substantially contributing to climate change. The correlation between industrial activity, carbon dioxide levels, and a warming planet is supported by numerous scientific inquiries. This connection traces back to the transformative period of industrialization, which marked the beginning of a distinct rise in global temperatures largely due to man-made factors.

From the Industrial Revolution to the Carbon Dioxide Boom

The industrial revolution stands as a pivotal chapter in human history, ushering in an era of economic progress, but also a critical turning point for the environment. During this time, the combustion of fossil fuels, such as coal, oil, and natural gas, exploded. This led to an unprecedented influx of carbon dioxide and other greenhouse gases into the atmosphere. The concentration of carbon dioxide alone has risen dramatically, correlating directly with industrial advancements and the resulting energy demands.

In response, we’ve witnessed the Earth’s average temperatures climb, as greenhouse gases trap solar energy, creating a warming effect known as the greenhouse effect. This surge in temperature, which has only intensified with time, finds its roots in the emissions trail left by industrialization, as evidenced by the clear data:

Year Carbon Dioxide Concentration Global Temperature Anomaly
Pre-Industrial Revolution ~280 ppm 0°C (base level)
Post-Industrial Revolution Significant Increase Rise corresponding to CO2 increase

Deforestation and the Role of Forests as Carbon Sinks

While industrial emission of greenhouse gases has been significant, the concurrent loss of forests amplifies this climate challenge. Deforestation, driven by agricultural expansion, logging, and development, has reduced the planet’s capacity to absorb carbon dioxide. Forests serve as essential carbon sinks; they capture carbon dioxide from the atmosphere and store it in biomass—a natural process crucial for balancing the global carbon cycle.

The destruction of these forests has not only contributed to the rise in carbon dioxide but has also jeopardized biodiversity, disrupted ecosystems, and impaired the planet’s ability to mitigate the accelerating effects of climate change. The importance of preserving existing forests and promoting reforestation efforts is therefore critical to maintaining these natural carbon sinks, as demonstrated here:

Activity Impact on Forests Effect on Carbon Dioxide Levels
Deforestation Loss of Carbon Storage Increase in Atmospheric CO2
Afforestation Growth in Carbon Storage Reduction in Atmospheric CO2

The intertwined dynamics of the industrial revolution, carbon dioxide increase, deforestation, and the deterioration of forests carbon sinks compel us to reflect upon the human impact on our planet. It is clear that informed, deliberate actions are required to address the balance and health of our Earth’s climatic system.

Measuring Past Climates: Ice Cores, Tree Rings, and Sediment

Unlocking the mysteries of the Earth’s climatic past is an intricate science involving sophisticated past climate measurement techniques. Among the most compelling of these are the analysis of ice cores, the practice of dendrochronology, and the examination of sediment layers—each of these methods provides a unique glimpse into the planet’s climatic history.

Ice cores, drilled from the depths of polar ice sheets and mountain glaciers, serve as time capsules containing invaluable climate data. These long cylinders of ice are stratified, with each layer representing a year, or sometimes even a specific season. By measuring the gases trapped within these layers, scientists can deduce atmospheric conditions dating back hundreds of thousands of years.

Complementing ice cores, dendrochronology—the study of tree rings—provides insight into historical climate conditions. Each ring marks a year in the life of a tree, with the thickness of these rings correlating with the climatic variables such as precipitation and temperature during that year. Trees, therefore, stand as silent recorders of past climates, harboring secrets of historical weather patterns within their very core.

Similarly, the stratified sediment layers found at the bottoms of lakes, oceans, and other bodies of water can tell stories of climatic conditions. Each layer captures particles that settle from above, including pollen, ash from volcanic eruptions, and other debris, chronicling changes in the Earth’s environment over time.

Together, these natural archives form a robust framework for understanding climate trends throughout history. While the evidence points to a series of natural variations over the millennia, recent climate change is happening at a pace that far exceeds these historical rates. The following table showcases some of the key insights garnered from these different methods:

Method Duration Covered Climate Insights
Ice Cores Up to 800,000 years Atmospheric gas concentrations, temperature patterns
Dendrochronology Up to 10,000 years Annual resolution of precipitation, temperature abnormalities
Sediment Layers Millions of years Changes in vegetation, volcanic activity, and broader environmental shifts

These climate measurement methods not only delineate the natural cadence of Earth’s ancient climate shifts but also underscore the acceleration in warmth and volatility we are currently witnessing. The data derived from these natural recorders aid scientists in piecing together the intricate puzzle of Earth’s climatic narrative, offering an unparalleled historical context against which to measure ongoing climatic changes.

Deciphering past climates is more than academic exercise; it’s a crucial piece in understanding our future. By appreciating the natural rhythms and fluctuations recorded in ice, wood, and sediment, we can better grasp the scale of humanity’s impact on this delicate system and the pressing need for stewardship in the face of rapid climatic shifts.

Recent Decades: A Rapid Rise in Temperatures and Extreme Weather Events

The escalating trajectory of global temperatures in recent decades has set off a chain reaction, leading to a surge in extreme weather conditions. This climatic upheaval is most evident in the prevalence of record heatwaves and the escalation in hurricanes intensity, phenomena that have wrought havoc across the globe. As greenhouse gas levels continue to soar and ocean temperatures increase, these weather events reveal the stark reality of our warming planet.

Record Heatwaves and the Increasing Intensity of Hurricanes

Heatwaves of unprecedented frequency and intensity have become the new normal, with the term “record heatwave” now a recurring headline in weather reports. These scorching events not only smash long-standing temperature records but also exacerbate the intensity of hurricanes. Warmer ocean waters add fuel to storm systems, bolstering their destructive power and increasing their potential for calamity. The devastation wrought by these strengthened storms underscores the urgent need to address the root causes of this escalatory trend.

Sea Level Rise: Coastal Erosion and High-Tide Flooding

Another ominous indicator of our changing climate is the steady creep of sea level rise, which has surpassed a 1.6-inch increase in recent years. This relentless upward trend poses a dire threat to coastal regions, where the specter of coastal erosion looms large. The encroachment of the sea not only gnaws away at shorelines but also leads to more frequent and severe bouts of high-tide flooding, disrupting communities and ecosystems alike. Satellite observations have cataloged this phenomenon, offering irrefutable evidence of the acceleration in sea level rise and its implications for our planet’s future.

The shift in Earth’s climatic rhythm is not a subtle one; it is a persistent and accelerating drumbeat heralding a future of heightened extremes. It is within this understanding that the importance of vigorous and proactive climate action finds its place, urgently calling for meaningful change to curtail the far-reaching impacts on our world.

Changing Climate Patterns: Projections and Potential Futures

As we push forward into the future, understanding the potential scenarios that our current climate path may unveil is essential in informing eco-conscious global strategies. The rapid changes in our climate demand thorough examination of the causes and ardent commitment to solutions—a narrative of climate pattern projections that articulately conveys the urgency and scope of the issue at hand.

Scenarios of Continued Fossil Fuel Use

The continued reliance on fossil fuels paints a daunting picture of our planet’s future climate. Models adopted in the U.S. Climate Science Special Report project that if the current trajectory of emissions persists, we could see the global temperature soar to unprecedented levels. This stark rise would exacerbate the fossil fuel impact on climate, leading to further destabilization of natural ecosystems, more frequent and severe weather events, and a heightened challenge in mitigating climate change.

With current emissions patterns, future temperature projections indicate a planet that is significantly warmer, posing irrefutable risk to natural and human systems alike.

The Path to Net-Zero Emissions and Mitigating Climate Change

Conversely, the path to net-zero emissions offers a beacon of hope. It involves transforming the global economy, shifting energy sources, and adopting innovative green technologies. Achieving net-zero emissions is not simply idealistic but necessary to stave off the worst effects of climate change. Projections by the International Energy Agency (IEA) combined with robust civil activism hint at a future where the growth of renewables potentially aligns global warming with the lower end of the Paris Agreement’s recommendations.

Ultimately, achieving mitigating climate change and steering towards net-zero emissions hinges on commitment across all sectors. The imperative to act is undeniable, with the potential to reverberate positively across generations and lay the groundwork for a sustainable mode of human-environment interaction.

  • Adoption of renewables and reduction in fossil fuel reliance is paramount to mitigating climate change.
  • Net-zero emissions target may reverse current warming trends if global action is taken swiftly.
  • Climate activism and policy changes present opportunities for aligning with sustainable climate pattern projections.

Conclusion

Our journey through the history of Earth’s climate shows a world increasingly shaped by human hands. An enhanced **climate change understanding** reveals the undeniable urgency for **future climate action**. The evidence is clear: the past decade has echoed a strong signal of rapid climatic disturbance – from escalating greenhouse gas emissions to surges in global temperatures – ringing in an era where human influence is the dominant force behind climatic dynamics. If this decade taught us anything, it’s that timely and decisive policies are now critical to accommodate the accelerating planetary transformations.

As stewards of an imperiled environment, it falls upon us to craft a future that favors resilience over ruin. The data from NOAA and the IPCC, combined with the collective outcry from communities across the globe, bolster the case for rapid, systemic changes in our approach to energy, deforestation, and emissions. Only through a unified, ambitious global effort can we hope to steer our shared climate story towards a narrative of mitigation and sustainability, rather than one of unchecked disruption and irreparable loss.

Addressing climate change is no longer just an environmental challenge – it’s a moral imperative that spans across economies, societies, and nations. It calls for the harnessing of innovation, the mobilization of resources, and the empowerment of individuals and communities to enact change. Our future climate action will dictate the world we pass on to subsequent generations. Let’s ensure it’s one where balance with nature and the vitality of our planet is placed at the very heart of progress.

FAQ

How has the climate changed historically?

Throughout Earth’s history, there have been significant climatic shifts over time, including ice ages, warmer interglacial periods, and a marked warming trend in the last century due to human activities.

What factors have influenced Earth’s climatic history?

Earth’s climate has been shaped by a variety of factors, including variations in Earth’s orbit, volcanic activity, and changes in greenhouse gas concentrations. Recently, human-induced factors like the burning of fossil fuels and deforestation have become dominant.

How is the current climate change different from past variations?

The current phase of climate change, particularly global warming, is occurring much more rapidly than many past changes and is predominantly driven by human activities such as fossil fuel combustion and land-use changes.

Why are ice age cycles and solar variations important?

Ice age cycles and solar variations are natural processes that have historically driven changes in climate. These factors have led to long-term shifts in temperature and ecologies on Earth over millennia.

How has volcanic activity impacted climate in the past?

Volcanic activity has had significant climate impacts by releasing ash and gases into the atmosphere. These materials can temporarily cool the Earth by reflecting sunlight away from the planet’s surface, leading to colder climates.

What is the significance of a 2-degree increase in global temperatures?

A 2-degree increase in global temperatures is highly significant, as it is associated with considerable changes in weather patterns, rising sea levels, shrinking ice caps, and biodiversity loss, among other impacts.

How is today’s climate pattern changing compared to pre-industrial times?

Since the pre-industrial era, there has been a marked increase in global temperatures, mainly due to the rise in greenhouse gas emissions from human activities. This has led to rapid changes in climate patterns.

How do greenhouse gas emissions affect climate change?

Greenhouse gas emissions from human activities, such as burning fossil fuels and deforestation, contribute to the greenhouse effect, trapping more heat in the atmosphere and leading to global warming.

How do scientists measure past climates?

Scientists use various proxies to measure past climates, including ice cores that trap air bubbles from ancient atmospheres, tree ring patterns (dendrochronology), and sediment layers that can reveal historical environmental conditions.

What have recent decades revealed about climate change?

Recent decades have shown an accelerated rise in global temperatures, contributing to an increase in extreme weather events, such as heatwaves and hurricanes, as well as a concerning rate of sea level rise.

What are the future projections for climate patterns?

Future projections suggest that continued fossil fuel use will result in significant warming. However, achieving net-zero emissions may mitigate some effects of climate change and limit warming to safer levels.

What actions can help address future climate change?

Reducing greenhouse gas emissions, transitioning to renewable energy sources, protecting and restoring forests, and investing in climate-resilient infrastructure can all help mitigate future climate change.

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