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Climate change: the losers, the winners and how to adapt

Agriculture, health, transport : the few ‘winners’ of climate change 

with Edward Gérardeaux, HDR from INP Toulouse and Deputy Director of the Aïda research unit at CIRAD and Emmanuelle Quillérou, environmental and natural resources economist at the University of Western Brittany
On May 16th, 2023 |
5 min reading time
GERARDEAUX_Edward
Edward Gérardeaux
HDR from INP Toulouse and Deputy Director of the Aïda research unit at CIRAD
QUILLEROU_Emmanuelle
Emmanuelle Quillérou
environmental and natural resources economist at the University of Western Brittany
Key takeaways
  • Since the 1960s, global warming has reduced overall yields of maize, wheat and rice, and slowed agricultural productivity growth by 21%.
  • But global warming may also benefit some crops, as the global rise in atmospheric CO2 concentration stimulates photosynthesis.
  • Food insecurity will increase, particularly in sub-Saharan Africa, South Asia, and Central America, with +8 to +80 million people affected.
  • The Arctic Ocean will become ice-free in summer by 2050, which means that new shipping routes and natural resources will become available.
  • While some communities will benefit from global warming, the rest of the world will be negatively impacted.

More than 3 bil­lion people live in condi­tions that are extre­me­ly vul­ne­rable to cli­mate change1. The impacts are undoub­ted­ly catas­tro­phic for the natu­ral and human sys­tems in place today. Howe­ver, this glo­bal obser­va­tion hides a degree of varia­bi­li­ty. In par­ti­cu­lar, a few com­mu­ni­ties will bene­fit at the expense of many more citi­zens adver­se­ly affec­ted by cli­mate change.

What are the effects on food security ?

Let us first look at the effects of cli­mate change on crops : the latest IPCC report devotes a chap­ter to the sub­ject2. On a glo­bal scale, yields have increa­sed by a fac­tor of 2.5 to 3 since the 1960s thanks to agri­cul­tu­ral tech­niques (varie­ties, irri­ga­tion, fer­ti­li­sa­tion etc.). Over the same per­iod, glo­bal war­ming has redu­ced glo­bal yields of maize (-5.9%), wheat (-4.9%) and rice (-4.2%)3 and slo­wed agri­cul­tu­ral pro­duc­ti­vi­ty growth by 21%4. Bet­ween now and the end of the cen­tu­ry, yield declines will continue.

But these ave­rages hide regio­nal dis­pa­ri­ties. While the expec­ted effects are “more nega­tive than posi­tive” accor­ding to the IPCC, some regions are bene­fi­ting from cli­mate change : rough­ly spea­king, those where ave­rage annual tem­pe­ra­tures are cur­rent­ly below 10°C (the Arc­tic and Cen­tral Asia for example). 

Since the 1960s, war­ming has slo­wed agri­cul­tu­ral pro­duc­ti­vi­ty growth by 21%.

“The effects of cli­mate change on crops are nume­rous and it is dif­fi­cult to gene­ra­lise,” says Edward Gerar­deaux. First­ly, the glo­bal rise in atmos­phe­ric CO2 concen­tra­tion sti­mu­lates pho­to­syn­the­sis and the­re­fore increases bio­mass. “This well-known effect bene­fits cer­tain crops that use a par­ti­cu­lar pho­to­syn­the­sis mecha­nism : wheat, rice, pota­toes, etc.” adds Gerar­deaux. Ano­ther posi­tive effect is the increase in tem­pe­ra­ture. “In some tem­pe­rate regions, it reduces heat stress and extends the areas sui­table for culti­va­tion, for example towards the poles or at high alti­tudes,” conti­nues Edward Gerar­deaux. In cen­tral Mada­gas­car, in the High­lands (the most popu­la­ted region), rice culti­va­tion is faci­li­ta­ted by cli­mate change. Esti­ma­ted yields exceed +10% (+576 kg/ha) for the pes­si­mis­tic GHG emis­sion sce­na­rios5. “The same effect is expec­ted for high­land coun­tries such as Rwan­da or cer­tain areas of Kenya,” adds Edward Gerar­deaux. In recent decades, posi­tive impacts of cli­mate change have been obser­ved on the pro­duc­ti­vi­ty of maize and rice in Cen­tral Asia, maize and soy­beans in North Ame­ri­ca, and wheat in North Afri­ca, Nor­thern Europe and South-East Asia, and rice in Australia.

Conver­se­ly, rising tem­pe­ra­tures affect the pro­duc­ti­vi­ty of many plants in regions with higher tem­pe­ra­tures. It speeds up their growth and shor­tens their lifes­pan. Edward Gerar­deaux adds : “Beyond a cer­tain thre­shold, tis­sues are degra­ded and frui­ting bodies are ste­rile : this is par­ti­cu­lar­ly true for clus­ter-flo­we­ring plants like maize and rice”. This is com­poun­ded by varia­tions in rain­fall : rain­fall defi­cits, increa­sed extreme events, etc. Drought has alrea­dy cau­sed losses in 75% of culti­va­ted areas6, and the com­bi­ned effects of heat and drought have redu­ced glo­bal yields of maize (-11.6%), soy­bean (-12.4%) and wheat (-9.2%)7. These effects out­weigh the posi­tive impacts in many parts of the world. For example, millet yields have fal­len by 10–20%, and sorg­hum yields by 5–15% in West Africa.

What does this mean for glo­bal food secu­ri­ty ? Food inse­cu­ri­ty will increase, par­ti­cu­lar­ly in sub-Saha­ran Afri­ca, South and Cen­tral Asia and Cen­tral Ame­ri­ca (+8 to +80 mil­lion people affec­ted). “The posi­tive effects on agri­cul­ture are not able to com­pen­sate for this risk,” concludes Edward Gerar­deaux. “Some com­mu­ni­ties will see their situa­tion improve, but this will not bene­fit a very large region, espe­cial­ly as trade is more com­pli­ca­ted in these areas.”

Malaria

Let us now take the example of mala­ria, a vec­tor-borne disease cau­sed by para­sites of the genus Plas­mo­dium. The pre­va­lence of the disease depends on socio-eco­no­mic (health sys­tem, human beha­viour, etc.) and cli­ma­tic fac­tors. The vec­tor – the Ano­pheles mos­qui­to – needs ade­quate rain­fall to create egg-laying sites. The Plas­mo­dium para­site requires a sui­table tem­pe­ra­ture (around 20°C) to mul­ti­ply in the mos­qui­to8. Final­ly, tem­pe­ra­tures that are too high or variable alter transmission.

The result ? Vec­to­rial capa­ci­ty – the abi­li­ty of mos­qui­toes to trans­mit the para­site – has increa­sed in recent years, and rising ave­rage tem­pe­ra­tures make lar­ger geo­gra­phi­cal areas sui­table for trans­mis­sion9. But in West Afri­ca, the mala­ria trans­mis­sion sea­son will decrease due to redu­ced rain­fall, so the risk of disease is redu­ced due to cli­mate change10. Conver­se­ly, the vec­to­rial capa­ci­ty of the insect will increase in sub-Saha­ran Afri­ca, Asia, and South America.

Focus on the Arctic

“There is talk of a pos­sible ‘cold rush’,” says Emma­nuelle Quillé­rou. At the poles, the phy­si­cal effects of cli­mate change are more wides­pread and signi­fi­cant11. Cli­mate models show that a glo­bal ave­rage war­ming of 4°C trans­lates into an 8°C rise in land tem­pe­ra­tures in the Arc­tic, and it is like­ly that the ocean will become ice-free in sum­mer before 2050. As a result, new ship­ping routes and natu­ral resources become available.

By 2050, nor­thern sea routes could be 56% more acces­sible than today.

Bet­ween 2013 and 2019, mari­time traf­fic increa­sed by 25% and the dis­tance tra­vel­led by 75%. By 2050, the Nor­thern Sea Routes (Nor­thern Sea Route, Nor­th­west Pas­sages, and the Trans­po­lar Sea Route) could be 56% more acces­sible than today. There is a clear cor­re­la­tion bet­ween the decrease in sea ice extent (-13% per decade so far12) and the increase in mari­time traf­fic. Eco­no­mic fac­tors also play a major role. “This is main­ly due to the increase in domes­tic traf­fic in Rus­sia,” com­ments Emma­nuelle Quillé­rou. “But Chi­na and some shi­pow­ners like Maersk are posi­tio­ning them­selves as ‘pio­neers’ in their use of these routes for inter­na­tio­nal trade by tes­ting cros­sings.” Shi­pow­ners hope to avoid tra­di­tio­nal routes such as the Suez Canal and reduce the dis­tance bet­ween Asia and Europe by 40%. “Howe­ver, costs are not redu­ced by 40%, » cau­tions Emma­nuelle Quillé­rou. “Fuel consump­tion is higher than in warm waters, it is some­times neces­sa­ry to use an ice­brea­ker, navi­ga­tion is slo­wer, infra­struc­ture is very limi­ted and pas­sage rights may be requi­red by cer­tain coas­tal states such as Rus­sia.” Without consi­de­ring deve­lop­ments other than cli­mate change, cost reduc­tions com­pa­red to other ship­ping routes are esti­ma­ted at 5–16% today, 29% in 2030 and 37% in 205013.

Ano­ther oppor­tu­ni­ty is the exploi­ta­tion of natu­ral resources. Many fos­sil resources are exploi­ted in the region (oil, gas, mine­rals such as dia­monds, rare earths, zinc etc.), and Rus­sia has alrea­dy expan­ded the exploi­ta­tion of natu­ral resources – oil and gas – in the Yamal and Gydan penin­su­las. The mel­ting of the ice increases the time frame in which these resources can be exploi­ted and acces­sed. 90 bil­lion bar­rels of oil, 1669 bil­lion cubic feet of natu­ral gas and 44 bil­lion bar­rels of LNG could be avai­lable in the future. “The exploi­ta­tion of natu­ral resources is more com­pli­ca­ted than elsew­here because of the extreme cli­ma­tic condi­tions. The mel­ting per­ma­frost des­ta­bi­lises the soil and requires the construc­tion of even more expen­sive infra­struc­ture,” warns Emma­nuelle Quillé­rou. “Lloyd’s, one of the lar­gest insu­rance com­pa­nies and a refe­rence in the field, has been refu­sing to insure cer­tain ope­ra­ting acti­vi­ties in the Arc­tic since 2012, as the asso­cia­ted finan­cial risks are dee­med too great. This has sent a very clear signal. Shell has per­sis­ted in the Arc­tic lon­ger than Total and BP, but ended up stop­ping ope­ra­tions ini­tia­ted in the 2000s, as the mis­ma­na­ge­ment of an oil spill put the brakes on ope­ra­tions.” Des­pite the oppor­tu­ni­ties, the increa­sed costs of com­mer­cial exploi­ta­tion of resources and ship­ping routes are hol­ding back the rush so far.

The rush towards the cold poses signi­fi­cant risks for cli­mate change miti­ga­tion. “A sharp increase in the level of eco­no­mic acti­vi­ty in the Arc­tic could not only gene­rate hea­vy pol­lu­tion of the natu­ral envi­ron­ment but also dis­rupt the fra­gile social and diplo­ma­tic balance in the region,” concludes Emma­nuelle Quillé­rou. “The safe­guards in place are still too limi­ted to limit the impacts on the natu­ral polar envi­ron­ment and the­re­fore on glo­bal cli­mate change.” While the region is alrea­dy high­ly expo­sed to cli­mate risk, redu­cing risks – inclu­ding new ones such as increa­sed pol­lu­tant emis­sions or cultu­ral and marine eco­sys­tem impacts – through contain­ment stra­te­gies is essen­tial in the face of the ‘cold rush’.

Anaïs Marechal 
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