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Southland, where sunshine drops sharply to 1, hours per annum, lies on the northern fringe of a broad zone of increasing cloudiness. Four hundred miles further to the south at Campbell Island the sunshine has the extremely low value of hours per annum. A pleasant feature of the New Zealand climate is the high proportion of sunshine during the winter months. To eliminate the effect of varying day-length the summer and winter sunshine at a few selected stations have been expressed as a percentage of the possible sunshine.
As these figures indicate, there is a marked increase in cloudiness in the North Island in winter, but little seasonal change in the South Island, except in Southland. The following table provides a brief summary of the main climatological elements for selected locations. A feature of the seasonal pattern of temperature for New Zealand is the near symmetry about either the hottest summer months or the coldest winter months.
In other words the summer-winter decline is an almost identical reversal of the winter-summer rise. This shows up clearly when temperatures for climatological stations are averaged month by month. The first two months of the calendar year, the summer months of January and February, display the same average temperature, that of This temperature is the highest average for any month, being approached by only the December average of Once February is past a decline sets in, the estimated average New Zealand temperature falling by 2.
Thereafter, successive inter-monthly temperature drops of 4. Progressing through and past July the temperature steadily rises, the increments being successively, 1. The following diagram illustrates the seasonal temperature pattern. Year — Rainfall was above average, mainly by about 25 per cent, in the Auckland provincial district, North Taranaki, Manawatu and Wellington, Nelson and most of Marlborough, and Central Otago.
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In the Taupo - Rotorua - Tauranga area totals were from 50 to 90 per cent above average. A record wet year was experienced over most of the Bay of Plenty and Nelson and also in parts of Marlborough; especially notable were the record totals for Tauranga 81 in. In a few areas it was drier than normal by more than 10 per cent — the Southland plain, Fiordland, the Kaikoura coast, part of southern Wairarapa, and about the Ruahine Range.
Even allowing for some uncertainties in the temperature data available before , it seems very likely that was the warmest year experienced since instrumental observations were first made in New Zealand in The whole period to was notable for the persistence of above-average temperatures, and it was easily the warmest nine years in the century of observations. Highest departures in were recorded over the North Island and lowest departures in parts of Marlborough and coastal districts of Otago and Southland.
It was appreciably sunnier than average in western districts of both islands and also in Canterbury, with increases exceeding hours on the West Coast. By contrast, it was cloudier than normal east of the main ranges in the North Island and also in Bay of Plenty, with hours less sunshine than average in the latter area. January and February were both sunny months and January was also unusually warm. Welcome rains in January relieved the drought situation which had developed in the area between North Canterbury and Hawke's Bay during the last quarter of February was a dry month and it was not until the beginning of March that rain brought an end to the drought in Northland.
The autumn months of March, April, and May were particularly wet in the Auckland provincial district, Nelson, and Marlborough. Elsewhere rainfall was adequate, and as May was unusually mild, conditions were favourable for farming. April was notable for a violent storm at mid month, with exceptionally strong winds and widespread damage, especially over the North Island. Flooding was reported during autumn in parts of Bay of Plenty and Northland.
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Winter temperatures over the whole country were the mildest for about 50 years and this was especially appreciated in the South Island, where pasture growth commenced early and stock wintered well. In parts of the North Island the ground was too wet. Lambing commenced under favourable conditions. Spring was marked by further very wet weather in the Bay of Plenty, especially in October. Here and in Waitomo—Taumarunui the ground was too wet at times, but generally it was a good season for farmers.
On the morning of 8 October westerly winds reached hurricane force over the Hauraki Plains and Franklin County, damaging many houses and uprooting trees. In the South Island December was sunny and dry — too dry for pastures in some areas. The persistently wet weather over the Bay of Plenty continued, and in this area the ground remained too wet. Elsewhere in the North Island it was a good month for pasture growth, in spite of exceptionally high rainfall in Gisborne and parts of Hawke's Bay.
The observations from which the following summary was compiled for the year were taken at hours New Zealand standard time, i. For the mean sea-level pressure values in millibars at hours New Zealand standard time were: Auckland When New Zealand was discovered by Europeans in it was found to be inhabited by a race of Polynesians called Maoris, who had migrated to these islands at least years previously.
It is generally accepted that the Maoris came originally from South-East Asia, whence, as proto-Polynesians, they moved eastwards from island to island until they reached the eastern Pacific, where they settled the islands now known collectively as Polynesia. From Polynesia the ancestors of the Maori sailed south-west in ocean-going canoes to reach New Zealand and these voyages were probably spread over several generations, perhaps several centuries. Oral Maori history and genealogy support the view that there was a final wave of migration of considerable magnitude about a.
Adapting themselves to a new physical environment, in isolation from the outside world, the Maoris produced forms of social and economic organisation and material culture which were significantly different from their Polynesian prototypes. Coming from tropical latitudes, the Maoris mainly confined themselves to the warmer North Island, and when discovered by Europeans were in a high state of neolithic civilisation, with marked superiority in the arts of wood carving and military engineering.
Their principal social unit was the family group, and from combinations of the numerous groups were formed the subtribes and tribes. They had highly developed social and ritualistic customs, and their system of land tenure and methods of cultivation were communal within the subtribes. Inter-tribal and intra-tribal warfare was common, and as individuals they displayed exceptional courage and intelligence. The immediate effect of European contacts on the Maoris was the outburst of a series of tribal wars waged with greater ferocity and a vastly greater loss of life than was customary in pre-European tribal engagements.
The high mortality could, of course, be credited to the acquisition of a more lethal weapon, the musket. The advantage lay originally with the coastal tribes as a result of their earlier contact with Europeans, the wars continuing until all tribes were equally well armed. These wars were later followed by wars against the colonists, but after the story has been one of unbroken peace between Maoris and Europeans.
The introduction of European diseases and firearms, and the impact of European civilisation on the traditional way of life and customs of the Maoris, had such an adverse effect that their numbers must have been reduced by over half during the nineteenth century. However, the virility of the race gradually asserted itself, and from the beginning of the twentieth century the Maori population has been rapidly increasing. Other island groups, such as the Cook Islands, Niue Island, and the Tokelau Islands, had also long been inhabited by Polynesians from various successive migrations extending over considerable periods prior to their discovery by Europeans.
Tasman had left Batavia on 14 August , and, after having discovered Tasmania, he steered eastward and sighted the west coast of the South Island, described by him as a high mountainous country.
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Sailing north, he had the misfortune to come into conflict with the Maoris at Golden Bay, on the north coast of the South Island, so that, though he continued his northward journey until he reached the northern tip of the country, he did not again attempt to land.