Jump to content
Main menu
Main menu
move to sidebar
hide
Navigation
Main page
Recent changes
Random page
Help about MediaWiki
Special pages
ClimateKG
Search
Search
English
Appearance
Create account
Log in
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Contributions
Talk
Editing
IPCC:AR6/WGII/Chapter-16
(section)
IPCC
Discussion
English
Read
Edit source
View history
Tools
Tools
move to sidebar
hide
Actions
Read
Edit source
View history
General
What links here
Related changes
Page information
In other projects
Appearance
move to sidebar
hide
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
==== 16.2.3.8 Economic Impacts ==== <div id="h3-15-siblings" class="h3-siblings"></div> Since the AR5, there has been significant progress regarding the identification of economic responses to weather fluctuations: evidence has increased that ''extreme weather events'' such as tropical cyclones, droughts, and severe fluvial floods have not only caused substantial immediate direct economic damage ( ''high confidence'' , see âCoastal SystemsâDamages, Table SM16.23, âWater distributionâReductions in water availability + induced damages and fatalitiesâ, Table SM16.23, and âWater distributionâFlood-induced economic damagesâ, Table SM16.22) but have also reduced economic growth in the short term (year of, and year after event) ( [[#Strobl--2011|Strobl, 2011]] ; [[#Strobl--2012|Strobl, 2012]] ; [[#Fomby--2013|Fomby et al., 2013]] ; [[#Felbermayr--2014|Felbermayr and GrĂśschl, 2014]] , Loyaza et al. 2012) ( ''high confidence'' ) as well as in the long term (up to 10â15 years after event) ( ''medium confidence'' ) ( [[#Hsiang--2014|Hsiang and Jina, 2014]] ; [[#Berlemann--2016|Berlemann and Wenzel, 2016]] ; [[#Berlemann--2018|Berlemann and Wenzel, 2018]] ; [[#Krichene--2020|Krichene et al., 2020]] ; [[#Tanoue--2020|Tanoue et al., 2020]] , see âOther societal impactsâMacroeconomic outputâ, Table SM16.23). Short- and long-term reductions of economic growth by ''extreme weather events'' affect both developing and industrialised countries, but have been shown to be more severe in developing than in industrialised economies, thereby increasing inequality between countries ( ''high confidence'' , see âOther societal impactsâBetween-country inequalityâ, Table SM16.23). Further, ''extreme weather events'' have increased within-country inequality since poorer people are more exposed and suffer relatively higher well-being losses than richer parts of the population ( ''medium confidence'' , see âOther societal impactsâWithin-country inequalityâ, Table SM16.23). Going beyond ''extreme weather events'' , economic production depends nonlinearly on temperature fluctuations: below a certain threshold temperature, economic production increases with temperature, whereas it decreases above a certain threshold temperature ( ''high confidence'' ) ( [[#Burke--2015|Burke et al., 2015]] ; [[#Pretis--2018|Pretis et al., 2018]] ; [[#Kalkuhl--2020|Kalkuhl and Wenz, 2020]] ; [[#Kotz--2021|Kotz et al., 2021]] ). So far, there are few individual studies attributing observed economic damages to long-term climate change except for damages induced by river flooding, droughts and tropical cyclones (see âCoastal systemsâDamagesâ, âWater distributionâFlood-induced damagesâ, and âWater distributionâReduction in water availability + induced damages and fatalitiesâ, Table SM16.22). In addition, the empirical findings on the sensitivity of macroeconomic development to weather fluctuations and ''extreme weather events'' have been used to estimate the cumulative effect of historical warming on long-term economic development (see âOther societal impactsâMacroeconomic outputâ, Table SM16.22): anthropogenic climate change is estimated to have reduced gross domestic product (GDP) growth over the last 50 years, with substantially larger negative effects on developing countries and in some cases positive effects on colder industrialised countries ( ''low confidence'' ) ( [[#Diffenbaugh--2019|Diffenbaugh and Burke, 2019]] ). Globally, between-country inequality has decreased over the last 50 years. Climate change is estimated to have substantially slowed down this trend, that is, increased inequality compared with a counterfactual no-climate-change baseline ( ''low confidence'' ) ( [[#Diffenbaugh--2019|Diffenbaugh and Burke, 2019]] ). On a regional level, decreasing rainfall trends in Sub-Saharan Africa may have increased the GDP per capita gap between Sub-Saharan Africa and other developing countries ( ''low confidence'' ) ( [[#Barrios--2010|Barrios et al., 2010]] ). Overall, more research is needed on the impact channels through which ''extreme weather events'' and weather variability can hinder economic development, especially in the long term. <div id="16.2.3.9" class="h3-container"></div> <span id="social-conflict"></span>
Summary:
Please note that all contributions to ClimateKG may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
ClimateKG:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)
Search
Search
Editing
IPCC:AR6/WGII/Chapter-16
(section)
Add languages
Add topic