Effects of climate change on livestock

[6][7] This causes both mass animal mortality during heatwaves, and the sublethal impacts, such as lower quantity of quality of products like milk, greater vulnerability to conditions like lameness or even impaired reproduction.[3] While some areas which currently support livestock animals are expected to avoid "extreme heat stress" even with high warming at the end of the century, others may stop being suitable as early as midcentury.[3]: 750  In general, sub-Saharan Africa is considered to be the most vulnerable region to food security shocks caused by the impacts of climate change on their livestock, as over 180 million people across those nations are expected to see significant declines in suitability of their rangelands around midcentury.[3]: 747  Much like how climate change is expected to increase overall thermal comfort for humans living in the colder regions of the world,[6] livestock in those places would also benefit from warmer winters.[2] Across the entire world, however, increasing summertime temperatures as well as more frequent and intense heatwaves will have clearly negative effects, substantially elevating the risk of livestock suffering from heat stress.Under the climate change scenario of highest emissions and greatest warming, SSP5-8.5, "cattle,sheep, goats, pigs and poultry in the low latitudes will face 72–136 additional days per year of extreme stress from high heat and humidity".Historically, livestock in these conditions were considered less vulnerable to warming than the animals in outdoor areas due to inhabiting insulated buildings, where ventilation systems are used to control the climate and relieve the excess heat.[19] In the United States alone, economic losses caused by heat stress in livestock were already valued at between $1.69 and $2.36 billion in 2003, with the spread reflecting different assumptions about the effectiveness of contemporary adaptation measures.[3]: 748 A range of climate change adaptation measures can help to protect livestock, such as increasing access to drinking water, creating better shelters for animals kept outdoors and improving air circulation in the existing indoor facilities.[23] Insufficient supply or quality of either leads to a decrease in growth and reproductive efficiency in domestic animals, especially in conjunction with the other stressors, and at worst, may increase mortality due to starvation.Consequently, Iranian rangelands support over twice their sustainable capacity, and this leads to mass mortality in poor years, such as when around 800,000 goats and sheep in Iran perished due to the severe 1999 − 2001 drought.96% of overall forage growth on such prairies stems from just six plant species, and they become 38% more productive largely in response to the increased CO2 levels, yet their nutritious value to livestock also declines by 13% due to the same, as they grow less edible tissue and become harder to digest.[39] Similar response was observed in Stylosanthes capilata, another important forage species in the tropics, which is likely to become more prevalent with warming, yet which may require irrigation to avoid substantial losses in nutritional value.[3]: 748 Similarly, an older study found that if 1.1 °C (2.0 °F) of warming occurs between 2005 and 2045 (rate comparable to hitting 2 °C (3.6 °F) by 2050), then under the current livestock management paradigm, global agricultural costs would increase by 3% (an estimated $145 billion), with the impact concentrated in pure pasturalist systems.[14] Without a significant improvement in epidemiological control measures, what is currently considered an once-in-20-years outbreak of bluetongue would occur as frequently as once in five or seven years by midcentury under all but the most optimistic warming scenario.[3]: 747  Ixodes ricinus, a tick which spreads pathogens like Lyme disease and tick-borne encephalitis, is predicted to become 5–7% more prevalent on livestock farms in Great Britain, depending on the extent of future climate change.Even after conception, a pregnancy is less likely to be carried to term due to reduced endometrial function and uterine blood flow, leading to increased embryonic mortality and early fetal loss.Cattle eat less when they experience acute heat stress during hottest parts of the day, only to compensate when it is cooler, and this disbalance soon causes acidosis, which can lead to laminitis.Additionally, one of the ways cattle can attempt to deal with higher temperatures is by panting more often, which rapidly decreases carbon dioxide concentrations and increases pH."[2] Bovine neutrophil function is impaired at higher temperatures, leaving mammary glands more vulnerable to infection,[60] and mastitis is already known to be more prevalent during the summer months, so there is an expectation this would worsen with continued climate change.[64] Since more variable and therefore less predictable precipitation is one of the well-established effects of climate change on the water cycle,[65]: 85  similar patterns were later established across the rest of the United States,[66] and then globally.Yet, prolonged exposure to very hot and/or humid conditions will lead to consequences such as anhidrosis, heat stroke, or brain damage, potentially culminating in death if not addressed with measures like cold water applications.[78] Parasitic worms Haemonchus contortus and Teladorsagia circumcincta are predicted to spread more easily amongst small ruminants as the winters become milder due to future warming, although in some places this is counteracted by summers getting hotter than their preferred temperature.[63] Earlier, similar effects have been observed with two other parasitic worms, Parelaphostrongylus odocoilei and Protostrongylus stilesi, which have already been able to reproduce for a longer period inside sheep due to milder temperatures in the sub-Arctic.[8] One paper estimated that in Austria, at an intensive farming facility used to fatten up about 1800 growing pigs at a time, the already observed warming between 1981 and 2017 would have increased relative annual heat stress by between 0.9 and 6.4% per year.[80] Average daily temperatures of around 33 °C (91 °F) are known to interfere with feeding in both broilers and egg hens, as well as lower their immune response, with outcomes such as reduced weight gain/egg production or greater incidence of salmonella infections, footpad dermatitis or meningitis.Multiple studies show that dietary supplementation with chromium can help to relieve these issues due to its antioxidative properties, particularly in combination with zinc or herbs like wood sorrel.[92] By mid-2010s, indigenous people of the Arctic have already observed reindeer breeding less and surviving winters less often, as warmer temperatures benefit biting insects and result in more intense and persistent swarm attacks.They also become more susceptible to parasites spread by such insects, and as the Arctic becomes warmer and more accessible to invasive species, it is anticipated that they will come in contact with pests and pathogens they have not encountered historically.[94] Together with measures like a massive deployment of green technology, this pathway assumes animal-derived food will play a lower role in global diets relative to now.
Map of countries considered most and least vulnerable to adverse impacts of climate change on their grazing livestock. [ 1 ]
Multi-faceted impacts of climate change on livestock. [ 2 ]
Increased intensity of global climate change causes even greater increases of thermal heat index in Jamaican farm animals. High thermal heat index is one of the more widely used indicators of heat stress. [ 12 ]
Impacts of heat stress on livestock animals. [ 2 ]
This diagram shows a proposed design of a heat exchanger for indoor rearing facilities, whose installation would help to protect livestock from heat stress. [ 8 ]
Overgrazed vs. stable pasture in Fall River County , South Dakota.
Worldwide production of alfalfa, an important fodder plant.
Impacts of one possible scenario of climate change on agricultural costs between 2005 and 2045, under a range of assumptions about the role of CO2 fertilization effect and the effectiveness of adaptation strategies. [ 42 ]
A sheep infected with bluetongue virus.
Various pathologies which can be caused by heat stress, many specific to cattle. [ 2 ]
Serous exudate from udder in E. coli mastitis in cow (left), in comparison to normal milk (right).
All but two or three of the top 10 beef-producing countries are likely to see lower production with greater warming. [ 7 ]
Diagram of heat regulation in horses. [ 70 ]
Sheep are known for tolerating heat better than cattle.
Pig farm in Taiwan , in 2020.
Photo of an egg farm in New England , taken around 2009.
Greenhouse gas emissions from agricultureimpacts of climate changeclimate changetrillionadaptationeffects of climate changelivestock productionheat stressheatwaveslamenessreproductionanimal feedCO2 fertilization effectparasitesvector-borne diseasessub-Saharan Africafood securityrangelandshuman development indexnational resiliencepastoralismfresh watercalorieproteinnet zerosubsidiesclimate change scenarioSSP5-8.5JamaicaCaribbeanruminantsbroilerslayer hensventilationmidlatitudeheat strokesyncopeheat crampsorgan dysfunction2003 European heat waveBrittanyPays-de-la-Loirerespiratorysweatingmetabolic disordersketosisketonecatabolizingantioxidantenzymeoxidative stressantioxidantschromiumimmune systemvaccinationclimate change adaptationFall River Countyforagesoybeanssoybeanalfalfatall fescueirrigationextreme weatherwater securityprecipitationZimbabweclimate change scenariosfreshwaterwater scarcityglacierprairiesGuinea grassligninStylosanthesdeforestationClimate change and infectious diseasesRift Valley feverEl NinohelminthsfecundityCulicoides imicolabluetongue virusIxodes ricinusLyme diseasetick-borne encephalitisleptospirosisTsetse fliestrypanosomashellfishFarmed fishtambaquiEthiopiadeveloping countriesMediterraneancow milkintensive farmingorganic farmingUnited StatesNebraskaBrahman cattlespermatogenesisspermatozoaconceptioncorpus luteumovarianoocyteendometrialuterinemetabolismalbuminadipose tissuelipidosisexudateE. coliruminalacidosislaminitiscarbon dioxidealkalosisbicarbonateurinationulcerswhite line diseasemastitisneutrophilmammary glandsCalliphoraRhipicephalus microplustemperateOstertagia ostertagiWyominghydrological cycleeffects of climate change on the water cycleSSP3-7.0bovinesprimateseccrine glandsapocrine glandshypertoniclatherinanhidrosisAfrican horse sicknessHendra virusflying foxRCP4.5Haemonchus contortusTeladorsagia circumcinctasub-ArcticTaiwanground-coupled heat exchangerevaporative coolercellulosewet bulb temperatureregenerative heat exchangersartificial lightnight shiftNew Englandacclimatizationimmune responsesalmonellafootpaddermatitismeningitiswhite meatvitamin Eluteinzeaxanthinglucosecholesterolantioxidativewood sorrelResveratrolJapanese quailsfertilityreindeerinvasive speciesShared Socioeconomic PathwaysIntergovernmental Panel on Climate Changegreen technologyeffects of climate change on agricultureenteric fermentationEconomic impacts of climate changeBibcodeScience of the Total EnvironmentThe GuardianScience NewsOur World in DataCosmosOremland RSHuman impact on the environmentAnthropoceneEcological footprintEnvironmental impact assessmentEnvironmental issueslist of issuesHuman impacton marine lifeList of global issuesImpact assessmentPlanetary boundariesSocial ecology (ethics)Causes of climate changeAgricultureanimal agriculturecannabis cultivationmeat productioncocoa productionpalm oilBitcoinCorporate behaviorDeforestation and climate changeEnergy industrybiofuelsbiodieselelectricityenergyfashionfracking (US)nuclear poweroil shalepetroleumreservoirstransportGenetic pollutionEnvironmental crimeExplosivesIndustrialisationManufacturingcleaning agentsconcretenanotechnologypesticidespharmaceuticals and personal careMarine lifefishingfishing down the food webmarine pollutionoverfishingMiningOverconsumptionOverdraftingOverexploitationOvergrazingParticulatesPollutionQuarryingTourismaviationshippingUrbanizationurban sprawlBiodiversity threatsbiodiversity lossdecline in amphibian populationsdecline in insect populationsrunaway climate changein the United StatesDefaunationDesertificationEcocideEcological crisisMultiple breadbasket failureEnvironmental insecurityEnvironmental issues in the United StatesCoral reefsExternalityForest diebackEnvironmental degradationErosionFreshwater cycleGreenhouse gas emissionsHabitat destructionHolocene extinctionNitrogen cycleLand degradationLand consumptionLand surface effects on climateLoss and damageLoss of green beltsOzone depletionResource depletionTropical cyclones and climate changeWater degradationWater pollutionAlternative fuel vehicle propulsionBirth controlCleaner productionClimate change mitigationCommunity resilienceCultured meatDecouplingEcological engineeringEnvironmental engineeringEnvironmental mitigationIndustrial ecologyMitigation bankingRecyclingReforestationRestoration ecologySustainabilitySustainable consumptionWaste minimizationCausesClimate systemGreenhouse effectCarbon dioxide in Earth's atmosphereScientific consensus on climate changeFossil fuelGreenhouse gasesCarbon accountingCarbon footprintCarbon leakagefrom agriculturefrom wetlandsWorld energy supply and consumptionHistory of climate change policy and politicsHistory of climate change scienceSvante ArrheniusJames HansenCharles David KeelingUnited Nations Climate Change conferencesEffects and issuesAbrupt climate changeAnoxic eventArctic methane emissionsArctic sea ice declineAtlantic meridional overturning circulationDroughtCoastal floodingHeat waveMarineUrban heat islandOceansacidificationdeoxygenationheat contentsea surface temperaturestratificationtemperatureRetreat of glaciers since 1850Sea level riseSeason creepTipping points in the climate systemTropical cyclonesWater cycleWildfiresBiomesMass mortality eventExtinction riskPlant biodiversityMulti-breadbasket failureChildrenCitiesCivilizational collapseDepopulation of settlementsDestruction of cultural heritageDisabilityEconomic impactsU.S. insurance industryFisheriesGenderHealthMental healthHuman rightsIndigenous peoplesInfectious diseasesMigrationPovertyPsychological impactsSecurity and conflictUrban floodingAfricaAmericasAntarcticaArcticAustraliaEuropeMiddle East and North AfricaSmall island countriesMitigationEconomics and financeCarbon budgetCarbon emission tradingCarbon offsets and creditsGold Standard (carbon offset standard)Carbon priceCarbon taxClimate debtClimate financeClimate risk insuranceCo-benefits of climate change mitigationEconomics of climate change mitigationFossil fuel divestmentGreen Climate FundLow-carbon economyNet zero emissionsCarbon capture and storageEnergy transitionFossil fuel phase-outRenewable energySustainable energycarbon sinksBlue carbonCarbon dioxide removalCarbon sequestrationDirect air captureCarbon farmingClimate-smart agricultureafforestationREDD and REDD+Land use, land-use change, and forestryNature-based solutionsIndividual action on climate changePlant-based dietBusiness actionClimate actionClimate emergency declarationClimate movementSchool Strike for ClimateDenialEcological griefGovernanceJusticeLitigationPoliticsPublic opinionAdaptation strategies on the German coastAdaptive capacityDisaster risk reductionEcosystem-based adaptationFlood controlManaged retreatResilienceVulnerabilityThe Adaptation FundNational Adaptation Programme of ActionCommunicationClimate Change Performance IndexClimate crisis (term)Climate spiralEducationMedia coveragePopular culture depictionsfictionvideo gamesWarming stripesGlasgow Climate PactKyoto ProtocolParis AgreementCooperative Mechanisms under Article 6 of the Paris AgreementNationally determined contributionsSustainable Development Goal 13United Nations Framework Convention on Climate ChangeGlobal surface temperatureInstrumental temperature recordSatellite temperature measurementAlbedoCarbon cycleatmosphericbiologicoceanicpermafrostCarbon sinkClimate sensitivityClimate variability and changeCloud feedbackCloud forcingFixed anvil temperature hypothesisCryosphereEarth's energy budgetExtreme event attributionFeedbacksGlobal warming potentialIllustrative model of greenhouse effect on climate changeOrbital forcingRadiative forcingClimate modelCoupled Model Intercomparison ProjectIntergovernmental Panel on Climate Change (IPCC)IPCC Sixth Assessment ReportPaleoclimatologyRepresentative Concentration PathwayGlossary