Impacts: Aotearoa’s changing climate
Image: Marcus Kauffman
Impacts
- Irreversible tipping points
- Feedback effects
- How hot could it get?
- ENSO: El Niño & La Niña
- Aotearoa’s changing climate
- – The forecast for Canterbury
- Rising sea levels
- – Canterbury sea levels
- Floods bigger & more often
- Ocean heating
- Ocean acidfication
- Ocean currents changing
- Wildfires bigger & more often
- Food insecurity
- Losing our glaciers
- Black carbon & ash on snow
- Animal & plants moving or dying
- Biodiversity vanishing
- Broken life-support systems
- More diseases and pandemics
- What will it cost us?
- Arctic ice loss impacts on NZ
- Antarctic sea ice loss impacts NZ
Home > Climate wiki > Impacts
Aotearoa’s changing climate
Summary
This century, climate change will alter New Zealand’s natural water cycle significantly. It will change how much rain and snow we receive, and at what time of year. It will change how much water is stored in the soil, snow, glaciers and aquifers. It will change how much water evaporates back to the atmosphere and how much flows through streams and rivers to the coast. And it will change the severity of droughts, floods and power shortages. – Deep South
Two-thirds of New Zealanders live in areas prone to flooding and rising sea levels – NZ Statistics, 2023
The number of people exposed to these hazards will increase as the climate changes. – p53 Draft Adaptation Plan for New Zealand, April 2022 (The final Plan was released August 2022)
- The oceans have absorbed ~93% of warming and are heating up 40% faster than previously estimated.
- The Southern Ocean, which plays a major role in Aotearoa’s climate, is almost entirely responsible for ‘uptaking almost all the planet’s ocean warming‘.
This Southern Ocean warming and its associated impacts are effectively irreversible on human time scales, because it takes millennia for heat trapped deep in the ocean to be released back into the atmosphere. – Huguenin et al, 2022
In the Southern Hemisphere climate models consistently predict an almost year-round poleward shift in mid-latitude westerly winds as a consequence of global warming. This poleward shift is most notable in the cool season, April–September. – Speer et al 2022
- The atmosphere holds
~ 7% more water for every 1°C warming; resulting in more intense precipitation, and more heat = more energy, winds are getting stronger. But:
The condensation of water vapour to make rain droplets releases heat. This, in turn, can fuel stronger convection in thunderstorms, which can then dump substantially more rain. This means that the intensity of extreme rainfall could increase by much more than 7% per degree of warming. What we’re seeing is that thunderstorms can likely dump about double or triple that rate – around 14–21% more rain for each degree of warming. – Dowdy et al, May 2024
- We already are experiencing extreme weather and increased evapotranspiration (10% more since 2003), leading to plant stress.
- Any drop in emissions won’t reverse warming or return us to a ‘normal’ climate as there’s a long lag time between emitting greenhouse gases and their effect (see ‘the last time there was this much carbon dioxide in the atmosphere‘).
- This is increasingly costly for all of us in a multitude of ways, from marine heatwaves that supercharge NZ storms and affect fish and bird populations, to drought, floods (rain and/or rivers), rising sea levels, ocean acidification, and loss of critical ecosystem services we need to survive.
Impacts
- Irreversible tipping points
- Feedback effects
- How hot could it get?
- ENSO: El Niño & La Niña
- Aotearoa’s changing climate
- – The forecast for Canterbury
- Rising sea levels
- – Canterbury sea levels
- Floods bigger & more often
- Ocean heating
- Ocean acidfication
- Ocean currents changing
- Wildfires bigger & more often
- Food insecurity
- Losing our glaciers
- Black carbon & ash on snow
- Animal & plants moving or dying
- Biodiversity vanishing
- Broken life-support systems
- More diseases and pandemics
- What will it cost us?
- Arctic ice loss impacts on NZ
- Antarctic sea ice loss impacts NZ
Home > Climate wiki > Impacts
Summary
2024 was Aotearoa New Zealand’s 10th-warmest year on record. The nationwide average temperature …was 13.25˚C, being 0.51˚C above the 1991-2020 annual average. Of New Zealand’s 10 warmest years on record, eight have occurred since 2013 – NIWA
This century, climate change will alter New Zealand’s natural water cycle significantly. It will change how much rain and snow we receive, and at what time of year. It will change how much water is stored in the soil, snow, glaciers and aquifers. It will change how much water evaporates back to the atmosphere and how much flows through streams and rivers to the coast. And it will change the severity of droughts, floods and power shortages. – Deep South
Two-thirds of New Zealanders live in areas prone to flooding and rising sea levels – NZ Statistics, 2023
The number of people exposed to these hazards will increase as the climate changes. – p53 Draft Adaptation Plan for New Zealand, April 2022 (The final Plan was released August 2022)
- The oceans have absorbed ~93% of warming and are heating up 40% faster than the was estimated ten years ago.
- The Southern Ocean, which plays a major role in Aotearoa’s climate, is almost entirely responsible for ‘uptaking almost all the planet’s ocean warming‘.
This Southern Ocean warming and its associated impacts are effectively irreversible on human time scales, because it takes millennia for heat trapped deep in the ocean to be released back into the atmosphere. – Huguenin et al, 2022
In the Southern Hemisphere climate models consistently predict an almost year-round poleward shift in mid-latitude westerly winds as a consequence of global warming. This poleward shift is most notable in the cool season, April–September. – Speer et al 2022
- The atmosphere holds
~ 7% more water for every 1°C warming; resulting in more intense precipitation, and more heat = more energy, winds are getting stronger. But:
The condensation of water vapour to make rain droplets releases heat. This, in turn, can fuel stronger convection in thunderstorms, which can then dump substantially more rain. This means that the intensity of extreme rainfall could increase by much more than 7% per degree of warming. What we’re seeing is that thunderstorms can likely dump about double or triple that rate – around 14–21% more rain for each degree of warming. – Dowdy et al, May 2024
- We already are experiencing extreme weather and increased evapotranspiration (10% more since 2003), leading to plant stress.
- Any drop in emissions won’t reverse warming or return us to a ‘normal’ climate as there’s a long lag time between emitting greenhouse gases and their effect (see ‘the last time there was this much carbon dioxide in the atmosphere‘).
- This is increasingly costly for all of us in a multitude of ways, from marine heatwaves that supercharge NZ storms and affect fish and bird populations, to drought, floods (rain and/or rivers), rising sea levels, ocean acidification, and loss of critical ecosystem services we need to survive.
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Some incoming radiation from the sun is reflected back into space due to the albedo effect of the cryosphere (ice caps, permafrost, glaciers) and atmospheric aerosols much of which, paradoxically, come from burning fossil fuels. About 89% of the retained excess heat is being absorbed by the oceans. The land takes up ~6%, the cryosphere absorbs ~4%—which is why it’s rapidly melting—and the remaining 1% is in the atmosphere.
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Temperature anomalies by Latitude for the first three months of 2026. Surface temperatures in the Southern Hemisphere were slightly more than 1°C higher compared to the period 1961-1980. This is because our hemisphere has less land and more ocean which takes up more heat. Despite our recent weather bombs, we’re experiencing less extreme weather and temperatures than the global average. Credit: Dr. Zack Labe Climate Central
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Click Figure 2 to be taken to the online portal. It contains multiple variables that allow you to explore how the climate is projected to change compared to historical base periods. Zoom in to explore what our future climate may look like in your area, based on the data used is the average (mean) of the values produced by each of the six climate models (Coupled Model Intercomparison Project Phase 6: CMIP6). NOTE: these projections are based on the modelling of available data. THEY ARE NOT PREDICTIONS. They are guides that will change as more data comes to hand. They do not adequately capture extreme events.
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Click the image above to be taken to the online portal. It contains multiple variables that allow you to explore how the climate is projected to change compared to historical base periods. Zoom in to explore what our future climate may look like in your area, based on the data used is the average (mean) of the values produced by each of the six climate models (Coupled Model Intercomparison Project Phase 6 or CMIP6). NOTE: these projections are based on the modelling of available data. THEY ARE NOT PREDICTIONS. They are guides that will change as more data comes to hand. They do not adequately capture extreme events.
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The IPCC Sixth Assessment Report: Impacts, Adaptation and Vulnerability, has placed nature at the forefront of its projections, recognising the critical life-supporting role of biodiversity in human health and well being as well as adapting to the impacts of climate change. The report paints a dire picture.
More information
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Polar regions are warming more than twice as fast as the rest of the planet, and this is changing our weather, which is strongly influenced by jetstreams including the polar vortex. Extreme hot or cold weather is often ‘stuck’ over one place for long periods.
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Clean ice and snow have a very high albedo, that is, they reflect up to 90% of solar radiation back into space The ocean is much darker, so it has a very low albedo, reflecting only about 6% of the incoming solar radiation and absorbing the other 94%, warming it much faster than the snow and ice (Fig. 4).As more ice forms, the water is cooler, leading to more ice forming, and so on, in a feedback effect. However,
Recent global temperature surge intensified by record-low planetary albedo – Science, 05 Dec. 2024 (Figs. 5 & 6)
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Image: Nathan Kurtz / NASA
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Image: Duspayev et al; Earth’s Sea Ice Radiative Effect from 1980 to 2023
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Evaporation occurs more frequently at higher temperatures because the water molecules are moving more quickly.
Condensation is the opposite. Water molecules bring heat energy with them, so the surface of the dust warms slightly while the temperature of the surrounding air cools slightly, allowing the droplets to condense. This is due to a fundamental law of thermodynamics: see the Clausius-Clapeyron Equation for describing a discontinuous phase transition between the different states (gas, liquid, solid) of water.Transpiration is the process by which plants ‘exhale’ water vapour through their stomata. Plants lose more than 90% of their water through transpiration. However, in the last 150 years as CO2 has been increasing, the density of stomata in some plants has dropped 34%. This is restricting the amount of water vapour the plants release. This has implications for the water cycle, especially in tropical rainforests, which by definition create rain largely through transpiration. This could also lead to more flooding:
Plants get more water-efficient and leak less underground soil moisture out through their pores in a carbon-rich atmosphere. Add this up over billions of leaves in very sunlit, leafy places, especially the tropics, and it means there is a bunch more soil moisture stored up underground, so much so that climate models predict rainfall events will saturate the ground and more rain will run off into rivers. – Ass. Professor Mike Pritchard, UCI
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Net emissions means gross (total) greenhouse gas emissions from all industrial activities, burning fossil fuels for energy, and agriculture, minus carbon saved and stored underground permanently via natural terrestrial and oceanic ecosystems.While every country also includes plantation forestry (in New Zealand, mostly radiata pine) as part of their carbon savings to offset gross emission, in reality, this is a very short term saving as there are huge carbon costs and risks associated with plantation forestry that are not fully accounted for.Most negative emissions technology to remove carbon from the atmosphere (Carbon Capture and Storage – see this website) also are included in the carbon ‘savings’ calculations for tax purposes. However the vast bulk of this engineering recycles carbon back into the atmosphere rather than permanently sequester carbon underground.‘Net emissions’ is thus an accounting term that countries use for reporting purposes, to calculate the balance of their emissions based on what they choose to include in those calculations. What’s left out of these equations still goes into the atmosphere.Global emissions continue to increase each year and dangerous tipping points are being breached, which means natural carbon sinks are now becoming sources of methane and carbon dioxide.
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RCPs or Representative Concentration Pathways were used in the 2013 IPCC Fifth Assessment Report to represent the concentration of greenhouse gases in the atmosphere, based on how these gases retain heat.- Heat is measured in watts per metre squared, written as W⋅m−2. In most graphs, the numbers 2.6, 4.5, 6.0, and 8.5 are W⋅m−2 however ‘W⋅m−2 ‘ is implied, and the four units are written instead as four scenarios: RCP2.6 etc. In some graphs, this is written without a decimal place: RCP26, RCP45 etc
RCPs were explicitly designed for the climate modelling community to explore the effects of different emissions trajectories or emissions concentrations (resulting in various Radiative Forcing values). The socio-economic characteristics used to define RCPs were not standardized, which made it difficult to map societal changes like population, education, and government policies to climate targets, such as keeping global warming well below 2°C.
SSPs address this by defining how societal choices can lead to changes in Radiative Forcing by the end of the century. As such, SSPs expand on RCPs to allow for a standardized comparison of society’s choices and their resulting levels of climate change.
To a large extent, earlier maps or graphs with ‘RCP8.5’ can be read as SSP5-8.5, often written as SSP585 or SSP85.
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- 2026: 2nd National Climate Change Risk Assessment, Climate Change Commission
- 2026: World Meteorological Association (WMO) Global Annual to Decadal Climate Update (2025-2029)
- 2025: Annual Climate Summary for 2024 Global Highlights, Copernicus
- 2024: Wasco et al; A systematic review of climate change science relevant to Australian design flood estimation, Hydrology and Earth Systems Sciences, 28|5 pp1251-1285 (Open access)
- Plain English explanation: Dowdy et al; Why are we seeing ‘supercharged thunderstorms’ in Australia? Australian Geographic
- 2023: Di Capua & Rahmstorf; Extreme weather in a changing climate, Environmental Research Letters 18
- 2023: Shaw & Miyawaki: Fast upper-level jet stream winds get faster under climate change, Nature Climate Change 30 Nov. (Open access)
- 2022: National adaptation plan; Ministry for the Environment
- 2022: Shaw et al; Stormier Southern Hemisphere induced by topography and ocean circulation, PNAS 119 |5
- Shaw, Guest post: Why the southern hemisphere is stormier than the northern Carbon Brief (open access plain English article on the above research)
- 2022: Interim guidance on the use of new sea-level rise projections; Ministry for the Environment
- 2022: Speer et al; Jet Stream Changes over Southeast Australia during the Early Cool Season in Response to Accelerated Global Warming, MDPI Climate 10 | 6 84 (open access)
- 2022: Heguenin et al; Drivers and distribution of global ocean heat uptake over the last half century, Nature Communications 13 | 4921 (open access)
- The Conversation: plain English article explaining the research
- ECan: Climate Change Canterbury
- New Zealand Climate Change Commission
- IPCC Sixth Assessment: Climate Change 2021: The Physical Science Basis
- NIWA: New Zealand’s climate
- NIWA: National Climate Centre
- NIWA: Climate change
- Ministry for the Environment: First national climate change risk assessment for New Zealand
- NIWA: Climate change for students
- NIWA: The impact of El Niño and La Niña on New Zealand’s climate
- Moana Project: forecasting marine heatwaves
- Deep South Science Challenge (NZ): Will your property become uninsurable?
- Deep South Science Challenge (NZ): Planning for coastal adaptation
- Deep South Science Challenge (NZ): How should the risks be shared?
- Deep South Science Challenge (NZ): Resilience to Natures’ Challenges: list with links to publications
- Deep South Science Challenge (NZ): Earth System Modelling and Predictions
- ICOS (Integrated carbon modelling systems): Covid-19
- 2022: Wang et al; Future Southern Ocean warming linked to projected ENSO variability, Nature Climate Change 12 pp649–654
- 2022: Chemke et al; The intensification of winter mid-latitude storm tracks in the Southern Hemisphere, Nature Climate Change 12, pp553–557
- 2021: Pascolini-Campbell et at; A 10 per cent increase in global land evapotranspiration from 2003 to 2019, Nature 593, pp543–547
- Tandon; Satellite data reveals impact of warming on global water cycle, Carbon Brief explanation of the research paper (free access)
- 2020: Frame et al; Climate
change attribution and the economic costs of extreme weather events: a
study on damages from extreme rainfall and drought, (New Zealand based) Climate Change 162, pp 781-797 - 2020: UN Emissions Gap Report
- 2020: Freedman & Kaplan; Firenadoes, ember attacks and megafires: Australia is seeing sci-fi weather. Washington Post, Feb 2020.
- 2020: Padrón et al; Observed changes in dry-season water availability attributed to human-induced climate change Nature Geoscience 13, pp477–481
- 2020 NOAA: Climate Change: Ocean Heat Content
- 2020 NOAA: Global Climate Report March 2020
- 2019 NIWA: New Zealand Fluvial and Pluvial Flood Exposure (part of the Deep South Challenge New Zealand)
- 2019 IPCC: The Ocean and Cryosphere in a Changing Climate: Summary for Policymakers
- 2019 UN Environment Programme: Emissions Gap Report
- 2019: WMO Statement on the State of the Global Climate in 2019, World Meteorological Organisation, WMO-No. 1248
- 2019: Salinger et al; The unprecedented coupled ocean-atmosphere summer heatwave in the New Zealand region 2017/18: drivers, mechanisms and impacts Environmental Research Letters 14/4
- 2019: Cheng et al; How fast are the oceans warming? Science 363/6423 pp128-129
- 2018: Ministry for the Environment: Climate
Change Projections for New Zealand: Atmosphere Projections Based on
Simulations from the IPCC Fifth Assessment, 2nd Edition. Wellington. - 2018 National Geographic: Half of the Great Barrier Reef Is Dead
- 2014 IPCC 5th assessment Report AR5: Australasia
- 2013/2014 IPCC 5th Assessment Report AR5 (full)

