Adapting to a changing climate
5 min read
Farmers are already experiencing the impact of climate change firsthand. Building resilience into your farm system will be key to coping with changing weather patterns, increased temperatures, and adverse events.
Farmers are used to dealing with the weather. However, extreme events like floods and drought are becoming more common. They regularly disrupt farming communities and affect farmers' livelihoods and daily farm management. The severity, scale, and frequency of these weather events will only increase over time. Alongside this, average temperatures will continue to rise, impacting pasture production and animal health, among other things.
Understanding how your farm might be affected by climate change and having an adverse event checklist or plan will help strengthen your farm system's resilience. In addition, this information can help you respond to requests from banks and insurance companies that are starting to examine how climate change risk and resilience could affect farm businesses.
When considering farm system changes or significant investments such as infrastructure, it is crucial to take a long-term perspective and consider adapting to a changing climate. The following questions might help:
DairyNZ is actively advocating for farmers as the Government develops and implements adaptation policies to address New Zealand’s response to climate change.
We also have a range of research projects underway looking at different aspects of adaptation, including:
New Zealand has already experienced around 1.1°C warming since the start of the 20th century. By 2040, there will likely be more extended dry spells, longer summers, shorter winters, and an ongoing increase in storms, wind and rainfall across large parts of the country.
The information below shows NIWA projections for temperature and sea level rise out to 2040.
Zone 1: Upper North Island
Warmer, drier, more hot days (over 25°C), low river flows reached earlier.
Rainfall little change - seasonal reduction in winter and spring, small increase in summer.
Fewer frosts.
Small decrease in extreme wind, ex-tropical cyclone intensity increases.
Sea level rise 0.36-0.71m (2090).
Zone 2: Western Lower North Island
Warmer, drier, more hot days (over 25°C), low river flows reached earlier.
Rainfall little changed - seasonal reduction in winter and spring, small increase in summer.
Fewer frosts.
Up to 10% increase in extreme wind, ex-tropical cyclone intensity increases.
Sea level rise 0.36-0.71m (2090).
Zone 3: Eastern Lower North Island
Warmer, very dry conditions increase, more hot days (over 25°C), very dry conditions increase except for high altitude Tararua Ranges.
Rainfall little changed - seasonal reduction in winter and spring, small increase in summer.
Fewer frosts.
Extreme wind speed increases up to 10%, intensity of ex-tropical cyclones increases.
Sea level rise 0.36-0.71m (2090).
Zone 4: Northern South Island
Warmer, -5 to +5 variance in number of dry days, increase in hot days (over 25°C).
Rainfall very wet days increase by 10% in Marlborough Sounds region. No change elsewhere.
Fewer frosts, decreased snow, snowline lifts from 1550m to 1550-1750m.
Extreme wind speeds increase up to 10%, intensity of ex-tropical cyclones increases.
Sea level rise 0.36-0.71m (2090).
Zone 5: Eastern South Island
Warmer, increase in hot days (over 25°C), fewer dry days/year on Canterbury Plains, more dry days in inland areas. Low river flow threshold reached earlier in the year.
Rainfall little change - small increases autumn-winter, small decreases in winter for Canterbury. -5% to +5% change in extreme precipitation. Largest decrease across Eastern Otago.
Fewer frosts, decreased snow. Snowline lifts from 1550m to 1550-1750m.
Extreme wind speeds increase up to 10%, intensity of ex-tropical cyclones increases.
Sea level rise 0.36-0.71m (2090).
Zone 6: Western and Southern South Island
Warmer, more hot days (over 25°C) - more in Central Otago, fewer in Fjordland, fewer dry days/year on central West Coast, +5 dry days/year for Kahurangi National Park and Southland.
Small increase in annual rainfall. Larger increase in winter. -5% to +5% change in extreme precipitation. Low river flow threshold reached earlier.
Fewer frosts, decreased snow. Snowline lifts from 1550m to 1700m-2000m.
Extreme wind speeds increase up to 10%, intensity of ex-tropical cyclones increases.
Sea level rise 0.36-0.71m (2090).
We also partner with other research organisations on this work and others, for example the Deep South National Science Challenge:
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