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brenthutch

IPCC sixth assessment report.

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Chapter 12 of the UN IPCC Sixth Assessment Report, Page 90 of Chapter 12 Climate Change Information for Regional Impact and for Risk Assessment.  It essentially charts the UN IPCC’s assessment of the odds that each type of extreme weather is due to climate change…there is no evidence of any increase or decrease, globally or by region, in the frequency, severity or extent of frost, mean precipitation, river floods, heavy precipitation and pluvial floods, landslides, aridity, hydrological drought, agricultural or ecological drought, fire weather or wildfires, mean wind speed, severe wind storms or tornados, tropical cyclones or hurricanes, sand and dust storms, snow glacial or ice sheets, heavy snowfall and ice storms, hail, snow avalanche, relative sea levels, coastal floods, coastal erosion, marine heatwaves, ocean acidity, air pollution weather or radiation at earth’s surface.

Isn’t it about time we stop labeling folks “climate change deniers” and instead refer to them as reality observers?

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Talk about cherry picking.

The whole point of that chapter is the availability of data to assess risk from climate change (you know, like insurance companies and farmers do -- they're capitalists).

A single chart showing where the best data is doesn't mean that confidence is lacking in those areas. It just says that's what people pay most attention to over the long run. And given just how big and varied the earth is, it'd be surprising if there were excellent data in all parts. Dry regions, and wet regions, historically pay attention to the amount of rain. Hot and cold regions historically pay attention to the temperature. Temperate regions don't really pay attention until it gets their attention.

The executive summary of the chapter starts with 

Quote

Climate change information is increasingly available and robust at regional scale for impacts and risk assessment. Climate services and vulnerability, impacts and adaptation studies require regional scale multi-decadal climate observations and projections.

Did you read the whole chapter, or did you go fishing for a piece of data that "supports" your contention that the change in planting climate regions in North America (which is what I have data for) is anecdotal.

Farmers in Europe are adjusting what crops they plant to new realities of temperature as well. Smaller scale farms that actually grow food are hurting. I suppose one answer is for us all to go to engineered and prepackaged food made out of corn and soybean waste, but that's not really a good answer. Soylent Green was a movie, not a prediction.

Wendy P.

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36 minutes ago, wmw999 said:

Did you read the whole chapter, or did you go fishing for a piece of data that "supports" your contention that the change in planting climate regions in North America (which is what I have data for) is anecdotal.

I am assuming this is some kind of rhetorical question, right?

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52 minutes ago, wmw999 said:

Did you read the whole chapter, or did you go fishing for a piece of data that "supports" your contention that the change in planting climate regions in North America (which is what I have data for) is anecdotal.

 

Wendy P.

Here is your evidence of climate change on US food production 

https://www.usda.gov/media/blog/2020/03/05/look-agricultural-productivity-growth-united-states-1948-2017
 

Funny how it keeps getting better, despite the alarmists’ predictions of disaster. Turns out more CO2 and a longer growing season = more food. Who would have thought ?

Edited by brenthutch

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1 hour ago, brenthutch said:

Here is your evidence of climate change on US food production 

https://www.usda.gov/media/blog/2020/03/05/look-agricultural-productivity-growth-united-states-1948-2017
 

Funny how it keeps getting better, despite the alarmists’ predictions of disaster. Turns out more CO2 and a longer growing season = more food. Who would have thought ?

yes I am sure " innovations in animal and crop genetics, chemicals, equipment and farm organization" have nothing to do with it.

 

Actually in that report, can you point where they state more CO2 is a contributing factor?

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To actually address the report, let's look at the summaries.  Items Brent wants to hide in bold.

Observed Warming and its Causes

Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase, with unequal historical and ongoing contributions arising from unsustainable energy use, land use and land-use change, lifestyles and patterns of consumption and production across regions, between and within countries, and among individuals (high confidence). 

Observed Changes and Impacts

Widespread and rapid changes in the atmosphere, ocean, cryosphere and biosphere have occurred. Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts and related losses and damages to nature and people (high confidence). Vulnerable communities who have historically contributed the least to current climate change are disproportionately affected (high confidence).

Current Progress in Adaptation and Gaps and Challenges

Adaptation planning and implementation has progressed across all sectors and regions, with documented benefits and varying effectiveness. Despite progress, adaptation gaps exist, and will continue to grow at current rates of implementation. Hard and soft limits to adaptation have been reached in some ecosystems and regions. Maladaptation is happening in some sectors and regions. Current global financial flows for adaptation are insufficient for, and constrain implementation of, adaptation options, especially in developing countries (high confidence).

Current Mitigation Progress, Gaps and Challenges

Policies and laws addressing mitigation have consistently expanded since AR5. Global GHG emissions in 2030 implied by nationally determined contributions (NDCs) announced by October 2021 make it likely that warming will exceed 1.5°C during the 21st century and make it harder to limit warming below 2°C. There are gaps between projected emissions from implemented policies and those from NDCs and finance flows fall short of the levels needed to meet climate goals across all sectors and regions. (high confidence) 

Future Climate Change, Risks, and Long-Term Responses

Continued greenhouse gas emissions will lead to increasing global warming, with the best estimate of reaching 1.5°C in the near term in considered scenarios and modelled pathways. Every increment of global warming will intensify multiple and concurrent hazards (high confidence). Deep, rapid, and sustained reductions in greenhouse gas emissions would lead to a discernible slowdown in global warming within around two decades, and also to discernible changes in atmospheric composition within a few years (high confidence). 

Climate Change Impacts and Climate-Related Risks

For any given future warming level, many climate-related risks are higher than assessed in AR5, and projected long-term impacts are up to multiple times higher than currently observed (high confidence). Risks and projected adverse impacts and related losses and damages from climate change escalate with every increment of global warming (very high confidence). Climatic and non-climatic risks will increasingly interact, creating compound and cascading risks that are more complex and difficult to manage (high confidence). 

Likelihood and Risks of Unavoidable, Irreversible or Abrupt Changes

Some future changes are unavoidable and/or irreversible but can be limited by deep, rapid and sustained global greenhouse gas emissions reduction. The likelihood of abrupt and/or irreversible changes increases with higher global warming levels. Similarly, the probability of low-likelihood outcomes associated with potentially very large adverse impacts increases with higher global warming levels. 

Adaptation Options and their Limits in a Warmer World

Adaptation options that are feasible and effective today will become constrained and less effective with increasing global warming. With increasing global warming, losses and damages will increase and additional human and natural systems will reach adaptation limits. Maladaptation can be avoided by flexible, multi-sectoral, inclusive, long-term planning and implementation of adaptation actions, with co-benefits to many sectors and systems. (high confidence) 

Carbon Budgets and Net Zero Emissions

Limiting human-caused global warming requires net zero CO2 emissions. Cumulative carbon emissions until the time of reaching net-zero CO2 emissions and the level of greenhouse gas emission reductions this decade largely determine whether warming can be limited to 1.5°C or 2°C (high confidence). Projected CO2 emissions from existing fossil fuel infrastructure without additional abatement would exceed the remaining carbon budget for 1.5°C (50%) (high confidence).

Mitigation Pathways

All global modelled pathways that limit warming to 1.5°C (>50%) with no or limited overshoot, and those that limit warming to 2°C (>67%), involve rapid and deep and, in most cases, immediate greenhouse gas emissions reductions in all sectors this decade. Global net zero CO2 emissions are reached for these pathway categories, in the early 2050s and around the early 2070s, respectively. (high confidence) {3.3, 3.4, 4.1, 4.5, Table 3.1} (Figure SPM.5, Box SPM.1)


Urgency of Near-Term Integrated Climate Action

Climate change is a threat to human well-being and planetary health (very high confidence). There is a rapidly closing window of opportunity to secure a liveable and sustainable future for all (very high confidence). Climate resilient development integrates adaptation and mitigation to advance sustainable development for all, and is enabled by increased international cooperation including improved access to adequate financial resources, particularly for vulnerable regions, sectors and groups, and inclusive governance and coordinated policies (high confidence). The choices and actions implemented in this decade will have impacts now and for thousands of years (high confidence). 

The Benefits of Near-Term Action

Deep, rapid and sustained mitigation and accelerated implementation of adaptation actions in this decade would reduce projected losses and damages for humans and ecosystems (very high confidence), and deliver many co-benefits, especially for air quality and health (high confidence). Delayed mitigation and adaptation action would lock-in high-emissions infrastructure, raise risks of stranded assets and cost-escalation, reduce feasibility, and increase losses and damages (high confidence). Near-term actions involve high up-front investments and potentially disruptive changes that can be lessened by a range of enabling policies (high confidence). 

Mitigation and Adaptation Options across Systems

Rapid and far-reaching transitions across all sectors and systems are necessary to achieve deep and sustained emissions reductions and secure a liveable and sustainable future for all. These system transitions involve a significant upscaling of a wide portfolio of mitigation and adaptation options. Feasible, effective, and low-cost options for mitigation and adaptation are already available, with differences across systems and regions. (high confidence)

 

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5 minutes ago, billvon said:

To actually address the report, let's look at the summaries.  Items Brent wants to hide in bold.

Observed Warming and its Causes

Human activities, principally through emissions of greenhouse gases, have unequivocally caused global warming, with global surface temperature reaching 1.1°C above 1850–1900 in 2011–2020. Global greenhouse gas emissions have continued to increase, with unequal historical and ongoing contributions arising from unsustainable energy use, land use and land-use change, lifestyles and patterns of consumption and production across regions, between and within countries, and among individuals (high confidence). 

Observed Changes and Impacts

Widespread and rapid changes in the atmosphere, ocean, cryosphere and biosphere have occurred. Human-caused climate change is already affecting many weather and climate extremes in every region across the globe. This has led to widespread adverse impacts and related losses and damages to nature and people (high confidence). Vulnerable communities who have historically contributed the least to current climate change are disproportionately affected (high confidence). {2.1, Table 2.1, Figure 2.2 and 2.3} (Figure SPM.1)

Current Progress in Adaptation and Gaps and Challenges

Adaptation planning and implementation has progressed across all sectors and regions, with documented benefits and varying effectiveness. Despite progress, adaptation gaps exist, and will continue to grow at current rates of implementation. Hard and soft limits to adaptation have been reached in some ecosystems and regions. Maladaptation is happening in some sectors and regions. Current global financial flows for adaptation are insufficient for, and constrain implementation of, adaptation options, especially in developing countries (high confidence).

Current Mitigation Progress, Gaps and Challenges

Policies and laws addressing mitigation have consistently expanded since AR5. Global GHG emissions in 2030 implied by nationally determined contributions (NDCs) announced by October 2021 make it likely that warming will exceed 1.5°C during the 21st century and make it harder to limit warming below 2°C. There are gaps between projected emissions from implemented policies and those from NDCs and finance flows fall short of the levels needed to meet climate goals across all sectors and regions. (high confidence) 

Future Climate Change, Risks, and Long-Term Responses

Continued greenhouse gas emissions will lead to increasing global warming, with the best estimate of reaching 1.5°C in the near term in considered scenarios and modelled pathways. Every increment of global warming will intensify multiple and concurrent hazards (high confidence). Deep, rapid, and sustained reductions in greenhouse gas emissions would lead to a discernible slowdown in global warming within around two decades, and also to discernible changes in atmospheric composition within a few years (high confidence). 

Climate Change Impacts and Climate-Related Risks

For any given future warming level, many climate-related risks are higher than assessed in AR5, and projected long-term impacts are up to multiple times higher than currently observed (high confidence). Risks and projected adverse impacts and related losses and damages from climate change escalate with every increment of global warming (very high confidence). Climatic and non-climatic risks will increasingly interact, creating compound and cascading risks that are more complex and difficult to manage (high confidence). 

Likelihood and Risks of Unavoidable, Irreversible or Abrupt Changes

Some future changes are unavoidable and/or irreversible but can be limited by deep, rapid and sustained global greenhouse gas emissions reduction. The likelihood of abrupt and/or irreversible changes increases with higher global warming levels. Similarly, the probability of low-likelihood outcomes associated with potentially very large adverse impacts increases with higher global warming levels. 

Adaptation Options and their Limits in a Warmer World

Adaptation options that are feasible and effective today will become constrained and less effective with increasing global warming. With increasing global warming, losses and damages will increase and additional human and natural systems will reach adaptation limits. Maladaptation can be avoided by flexible, multi-sectoral, inclusive, long-term planning and implementation of adaptation actions, with co-benefits to many sectors and systems. (high confidence) 

Carbon Budgets and Net Zero Emissions

Limiting human-caused global warming requires net zero CO2 emissions. Cumulative carbon emissions until the time of reaching net-zero CO2 emissions and the level of greenhouse gas emission reductions this decade largely determine whether warming can be limited to 1.5°C or 2°C (high confidence). Projected CO2 emissions from existing fossil fuel infrastructure without additional abatement would exceed the remaining carbon budget for 1.5°C (50%) (high confidence).

Mitigation Pathways

All global modelled pathways that limit warming to 1.5°C (>50%) with no or limited overshoot, and those that limit warming to 2°C (>67%), involve rapid and deep and, in most cases, immediate greenhouse gas emissions reductions in all sectors this decade. Global net zero CO2 emissions are reached for these pathway categories, in the early 2050s and around the early 2070s, respectively. (high confidence) {3.3, 3.4, 4.1, 4.5, Table 3.1} (Figure SPM.5, Box SPM.1)


Urgency of Near-Term Integrated Climate Action

Climate change is a threat to human well-being and planetary health (very high confidence). There is a rapidly closing window of opportunity to secure a liveable and sustainable future for all (very high confidence). Climate resilient development integrates adaptation and mitigation to advance sustainable development for all, and is enabled by increased international cooperation including improved access to adequate financial resources, particularly for vulnerable regions, sectors and groups, and inclusive governance and coordinated policies (high confidence). The choices and actions implemented in this decade will have impacts now and for thousands of years (high confidence). 

The Benefits of Near-Term Action

Deep, rapid and sustained mitigation and accelerated implementation of adaptation actions in this decade would reduce projected losses and damages for humans and ecosystems (very high confidence), and deliver many co-benefits, especially for air quality and health (high confidence). Delayed mitigation and adaptation action would lock-in high-emissions infrastructure, raise risks of stranded assets and cost-escalation, reduce feasibility, and increase losses and damages (high confidence). Near-term actions involve high up-front investments and potentially disruptive changes that can be lessened by a range of enabling policies (high confidence). 

Mitigation and Adaptation Options across Systems

Rapid and far-reaching transitions across all sectors and systems are necessary to achieve deep and sustained emissions reductions and secure a liveable and sustainable future for all. These system transitions involve a significant upscaling of a wide portfolio of mitigation and adaptation options. Feasible, effective, and low-cost options for mitigation and adaptation are already available, with differences across systems and regions. (high confidence)

 

I assume you'll agree that it is possible his copy didn't have this information. I think you need to cut him a little slack here.

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