Atmospheric analysis

NIWA has been using advanced scientific instruments to measure atmospheric trace gases and isotopes for over 50 years.

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    Mangaotama catchment

    Mangaotama catchment, Whatawhata, Waikato – win:win for farming and the environment The Mangaotama project is one of the few studies where the effects of land use have been experimentally manipulated and tested on a catchment scale. It’s centred on a 280-hectare model hill farm at the Whatawhata Research Centre near Hamilton, in the Mangaotama catchment (a tributary of the Waipa and Waikato Rivers).
  • Fact sheet for HPCF

    Three Cray supercomputers—Māui, Mahuika and Kupe—make up the High Performance Computing Facility.
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    Baseline Tables

  • Stream restoration for aquatic invertebrates

    Research Project
    Streams play a key role in the ecosystems of New Zealand’s unique landscape. They feed and link together freshwater sources, maintain good water quality and support habitats that sustain our biodiversity.
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    Understanding Natural Shellfish Colonisation Processes

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    Active shellfish reseeding

  • Restoring shellfish habitats in estuaries

    Research Project
    Changes to the local environment and over harvesting have damaged shellfish populations in many estuaries. These projects examine the most effective way to restore these habitats and allow healthy populations of shellfish to return.
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    Technical note: some points of detail about adjustments for Auckland

    Missing data 
    Breaks in the lines on the temperature graphs occur where there are missing data. For the purpose of this illustration, annual averages are calculated only where there is a complete year of monthly values available on the NIWA Climate Database. In the case of Albert Park, some data are missing due to persistent vandalism of equipment there.
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    Combining data from multiple sites in Auckland

    Temperature measurements made at three sites in Auckland over roughly the same period
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    Technical note: some points of detail on adjustments for Wellington

    Making adjustments when combining data from multiple sites in Wellington
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    Combining temperature data from multiple sites in Wellington

    Early temperature measurements were made at a site in Thorndon, but the site was relocated in 1928 to Kelburn: 120m higher
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    Why climate data sometimes need to be adjusted

    How do climate scientists identify a real temperature trend? For example, what happens if some temperature measurements were made on top of a hill and other measurements were at sea level?