3.1.3.b (Q164): Difference between revisions

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(‎Created claim: has the IPCC statement (P3): Sea level rise is unavoidable for centuries to millennia due to continuing deep ocean warming and ice sheet melt, and sea levels will remain elevated for thousands of years.)
(‎Changed claim: has the IPCC statement (P3): At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia.)
 
(11 intermediate revisions by the same user not shown)
Property / has the IPCC statement
 
Global mean sea level rise will continue in the 21st century (virtually certain), with projected regional relative sea level rise within 20% of the global mean along two-thirds of the global coastline. (English)
Property / has the IPCC statement: Global mean sea level rise will continue in the 21st century (virtually certain), with projected regional relative sea level rise within 20% of the global mean along two-thirds of the global coastline. (English) / rank
 
Normal rank
Property / has the IPCC statement: Global mean sea level rise will continue in the 21st century (virtually certain), with projected regional relative sea level rise within 20% of the global mean along two-thirds of the global coastline. (English) / qualifier
 
series ordinal: 2
Amount2
Unit1
Property / has the IPCC statement: Global mean sea level rise will continue in the 21st century (virtually certain), with projected regional relative sea level rise within 20% of the global mean along two-thirds of the global coastline. (English) / qualifier
 
Property / has the IPCC statement
 
The magnitude, the rate, the timing of threshold exceedances, and the long-term commitment of sea level rise depend on emissions, with higher emissions leading to greater and faster rates of sea level rise. (English)
Property / has the IPCC statement: The magnitude, the rate, the timing of threshold exceedances, and the long-term commitment of sea level rise depend on emissions, with higher emissions leading to greater and faster rates of sea level rise. (English) / rank
 
Normal rank
Property / has the IPCC statement: The magnitude, the rate, the timing of threshold exceedances, and the long-term commitment of sea level rise depend on emissions, with higher emissions leading to greater and faster rates of sea level rise. (English) / qualifier
 
series ordinal: 3
Amount3
Unit1
Property / has the IPCC statement
 
Due to relative sea level rise, extreme sea level events that occurred once per century in the recent past are projected to occur at least annually at more than half of all tide gauge locations by 2100 and risks for coastal ecosystems, people and infrastructure will continue to increase beyond 2100. (English)
Property / has the IPCC statement: Due to relative sea level rise, extreme sea level events that occurred once per century in the recent past are projected to occur at least annually at more than half of all tide gauge locations by 2100 and risks for coastal ecosystems, people and infrastructure will continue to increase beyond 2100. (English) / rank
 
Normal rank
Property / has the IPCC statement: Due to relative sea level rise, extreme sea level events that occurred once per century in the recent past are projected to occur at least annually at more than half of all tide gauge locations by 2100 and risks for coastal ecosystems, people and infrastructure will continue to increase beyond 2100. (English) / qualifier
 
series ordinal: 4
Amount4
Unit1
Property / has the IPCC statement: Due to relative sea level rise, extreme sea level events that occurred once per century in the recent past are projected to occur at least annually at more than half of all tide gauge locations by 2100 and risks for coastal ecosystems, people and infrastructure will continue to increase beyond 2100. (English) / qualifier
 
Property / has the IPCC statement
 
At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia. (English)
Property / has the IPCC statement: At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia. (English) / rank
 
Normal rank
Property / has the IPCC statement: At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia. (English) / qualifier
 
series ordinal: 5
Amount5
Unit1
Property / has the IPCC statement: At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia. (English) / qualifier
 
Property / has the IPCC statement: At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia. (English) / qualifier
 
Property / has the IPCC statement: At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia. (English) / qualifier
 
confidence level: unknown value
Property / has the IPCC statement
 
The probability and rate of ice mass loss increase with higher global surface temperatures. (English)
Property / has the IPCC statement: The probability and rate of ice mass loss increase with higher global surface temperatures. (English) / rank
 
Normal rank
Property / has the IPCC statement: The probability and rate of ice mass loss increase with higher global surface temperatures. (English) / qualifier
 
series ordinal: 6
Amount6
Unit1
Property / has the IPCC statement: The probability and rate of ice mass loss increase with higher global surface temperatures. (English) / qualifier
 
Property / has the IPCC statement
 
Over the next 2000 years, global mean sea level will rise by about 2– 3 m if warming is limited to 1.5°C and 2–6 m if limited to 2°C. (English)
Property / has the IPCC statement: Over the next 2000 years, global mean sea level will rise by about 2– 3 m if warming is limited to 1.5°C and 2–6 m if limited to 2°C. (English) / rank
 
Normal rank
Property / has the IPCC statement: Over the next 2000 years, global mean sea level will rise by about 2– 3 m if warming is limited to 1.5°C and 2–6 m if limited to 2°C. (English) / qualifier
 
series ordinal: 7
Amount7
Unit1
Property / has the IPCC statement: Over the next 2000 years, global mean sea level will rise by about 2– 3 m if warming is limited to 1.5°C and 2–6 m if limited to 2°C. (English) / qualifier
 
Property / has the IPCC statement
 
Projections of multi-millennial global mean sea level rise are consistent with reconstructed levels during past warm climate periods: global mean sea level was very likely 5–25 m higher than today roughly 3 million years ago, when global temperatures were 2.5°C–4°C higher than 1850–1900. (English)
Property / has the IPCC statement: Projections of multi-millennial global mean sea level rise are consistent with reconstructed levels during past warm climate periods: global mean sea level was very likely 5–25 m higher than today roughly 3 million years ago, when global temperatures were 2.5°C–4°C higher than 1850–1900. (English) / rank
 
Normal rank
Property / has the IPCC statement: Projections of multi-millennial global mean sea level rise are consistent with reconstructed levels during past warm climate periods: global mean sea level was very likely 5–25 m higher than today roughly 3 million years ago, when global temperatures were 2.5°C–4°C higher than 1850–1900. (English) / qualifier
 
series ordinal: 8
Amount8
Unit1
Property / has the IPCC statement: Projections of multi-millennial global mean sea level rise are consistent with reconstructed levels during past warm climate periods: global mean sea level was very likely 5–25 m higher than today roughly 3 million years ago, when global temperatures were 2.5°C–4°C higher than 1850–1900. (English) / qualifier
 
Property / has the IPCC statement
 
Further examples of unavoidable changes in the climate system due to multi-decadal or longer response timescales include continued glacier melt and permafrost carbon loss. (English)
Property / has the IPCC statement: Further examples of unavoidable changes in the climate system due to multi-decadal or longer response timescales include continued glacier melt and permafrost carbon loss. (English) / rank
 
Normal rank
Property / has the IPCC statement: Further examples of unavoidable changes in the climate system due to multi-decadal or longer response timescales include continued glacier melt and permafrost carbon loss. (English) / qualifier
 
series ordinal: 9
Amount9
Unit1
Property / has the IPCC statement: Further examples of unavoidable changes in the climate system due to multi-decadal or longer response timescales include continued glacier melt and permafrost carbon loss. (English) / qualifier
 
Property / has the IPCC statement: Further examples of unavoidable changes in the climate system due to multi-decadal or longer response timescales include continued glacier melt and permafrost carbon loss. (English) / qualifier
 

Latest revision as of 15:31, 18 May 2023

No description defined
Language Label Description Also known as
English
3.1.3.b
No description defined

    Statements

    instance of
    section
    0 references
    has the IPCC statement
    Sea level rise is unavoidable for centuries to millennia due to continuing deep ocean warming and ice sheet melt, and sea levels will remain elevated for thousands of years. (English)
    confidence level
    high confidence
    series ordinal
    1
    0 references
    Global mean sea level rise will continue in the 21st century (virtually certain), with projected regional relative sea level rise within 20% of the global mean along two-thirds of the global coastline. (English)
    series ordinal
    2
    confidence level
    medium confidence
    0 references
    The magnitude, the rate, the timing of threshold exceedances, and the long-term commitment of sea level rise depend on emissions, with higher emissions leading to greater and faster rates of sea level rise. (English)
    series ordinal
    3
    0 references
    Due to relative sea level rise, extreme sea level events that occurred once per century in the recent past are projected to occur at least annually at more than half of all tide gauge locations by 2100 and risks for coastal ecosystems, people and infrastructure will continue to increase beyond 2100. (English)
    series ordinal
    4
    confidence level
    high confidence
    0 references
    At sustained warming levels between 2°C and 3°C, the Greenland and West Antarctic ice sheets will be lost almost completely and irreversibly over multiple millennia. (English)
    series ordinal
    5
    spatial scope
    Greenland ice sheet
    West Antarctic Ice Sheet
    confidence level
    unknown value
    0 references
    The probability and rate of ice mass loss increase with higher global surface temperatures. (English)
    series ordinal
    6
    confidence level
    high confidence
    0 references
    Over the next 2000 years, global mean sea level will rise by about 2– 3 m if warming is limited to 1.5°C and 2–6 m if limited to 2°C. (English)
    series ordinal
    7
    confidence level
    low confidence
    0 references
    Projections of multi-millennial global mean sea level rise are consistent with reconstructed levels during past warm climate periods: global mean sea level was very likely 5–25 m higher than today roughly 3 million years ago, when global temperatures were 2.5°C–4°C higher than 1850–1900. (English)
    series ordinal
    8
    confidence level
    medium confidence
    0 references
    Further examples of unavoidable changes in the climate system due to multi-decadal or longer response timescales include continued glacier melt and permafrost carbon loss. (English)
    series ordinal
    9
    confidence level
    very high confidence
    high confidence
    0 references
     
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