This webpage provides a brief summary of climate and hydrological conditions in the region. This service is only updated during periods in which closer monitoring is required (regardless of time of the year), in recognition that we are in a dry spell of weather. It does not define an official council position on drought or drought declaration.
Most of the North Island and half of the South Island were extremely dry during the beginning of the year. The large spatial extension of the drought event last summer has been very unusual.
As a result, the Agriculture Minister declared a large scale adverse event for the entire North Island, and parts of the South Island, in March. The last large-scale adverse event classification for drought in New Zealand was in 2013.
The winter rain was insufficient for a full hydrological recovery. Some areas in the south of the Region had just over half of the long-term average rainfall for the season. This, combined with higher than average temperatures, is helping promote greater evapotranspiration from soil and plants in the lead up to summer.
The Wairarapa finished the hydrological year (1 June 2019 to 31 May 2020) with a rainfall deficit ranging between 100 and 200 mm from Masterton to the eastern coast, while the high elevation areas of the Tararuas finished the year with a deficit of around 1,000 mm.
Sustained rainfall is needed to restore and maintain the ‘normal’ hydrological balance. This ‘normal’ longer-term water balance is becoming increasingly hard to maintain due to climate change, and more unreliable weather patterns (see below).
A La Niña event has now developed, and should persist at least until the end of the year. A negative Indian Ocean Dipole is also expected during spring.
Even though the negative phases of these combined drivers are not necessarily associated with severe droughts in our region (differently to El Niño), they still tend to be associated with lower than average rainfall in the Wairarapa in spring (see NIWA climate drivers report for GWRC).
In summer, La Niñas tend to evolve to dry conditions in the west coast, with a predominant north-easterly flow bringing thunderstorms inland. A La Niña is normally accompanied by warm oceanic temperatures around New Zealand, which could also contribute to exacerbate the background warming signal from climate change, potentially pushing the seasonal temperatures well above average.
In short: there is a high likelihood that warm and dry meteorological conditions (compared to the seasonal average) may develop later in spring and early summer. This climate signal may exacerbate the hydrological deficit in our region that already exists after a dry winter.
Even though there is no forecast of a new major drought for the summer season ahead, the combination of these drivers could potentially lead to a new surge of dryness, low soil moisture, and low flow conditions by the end of the year.
With climate change, droughts are expected to become more severe and frequent in the Wellington region, particularly in the Wairarapa.
Even if international climate policy efforts successfully contain global warming under 1.5-2 degrees (the Paris Agreement’s ambition), it is important that we build water resilience and be prepared for a “new normal” climate pattern, significantly drier than in the past.
We note that the warming temperatures also mean that evapotranspiration is greatly increased. There is some evidence that our soils are getting drier, and ground water storage may be decreasing, in the long-term.
How different has recent rainfall/soil moisture been compared with the same time in previous years?
Click on the links below to see the relevant anomaly map
|Kapiti Coast (lowland)||Otaki at Depot|
|Kapiti Coast (high altitude)||Penn Creek at McIntosh|
|Porirua||Horokiri Stream at Battle Hill
|Wellington City||Kaiwharawhara Stream at Karori Reservoir|
|Hutt Valley (upper catchment)||Hutt River at Kaitoke Headworks|
|Upper Hutt||Upper Hutt at Savage Park||Upper Hutt at Savage Park AQ|
|Wainuiomata||Wanuiomata River at Wainui Reservoir|
|Wairarapa (high altitude)||Waingawa River at Angle Knob|
|Wairarapa Valley (north)||Kopuaranga River at Mauriceville|
|Wairarapa Valley (Masterton)||Ruamahanga River at Wairarapa College||Wairarapa College AQ|
|Wairarapa Valley (south)||Tauherenikau River at Racecourse||Tauherenikau River at Racecourse|
|Wairarapa (north-eastern hills)||Whareama River at Tanawa Hut||Whareama River at Tanawa Hut|
|Wairarapa (south-eastern hills)||Waikoukou at Longbush||Waikoukou at Longbush|