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Your host will collect all the Speeding Tickets at the end of the evening. A match occurs when a person you want to meet also wants to meet you again. We will send you the contact details of your matches the day after your Speed Dating event. The rest is up to you!
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You are invited to learn the art of Belly Dancing! Belly dancing is for all women of any age, size or fitness level and no experience in any dance form is necessary! Find out more about our classes around Auckland online. Visit the official website to find out more about our classes around Auckland. Level One is back at the home of live comedy - more comedians , more seats, more laughs still with hyper-hygiene and contact tracing protocols.
And all week , all month we are celebrating our 23rd birthday in Mocktober at The Classic. Thursday 29 October Get directions. Find out about listing on Aucklandnz. Powered by. In this area. Spend the morning exploring Auckland City on our small group tour and in the afternoon, taste some of New Zealand's best wine, enjoy local food and drink in the dramatic scenery of Auckland's west coast. Adventure Capital offer the most popular cycling experiences in Auckland. We have self-guided and guided experiences to suit almost all ages and abilities from our store located within walking distance of CBD hotels and cruise terminals.
Earthquakes during —Earthquakes did not cause any appreciable damage in The most noteworthy event was the swarm of small earthquakes, centred near Puru in the Coromandel Peninsula, that began in August and persisted for more than a month. There were several hundred shocks, many of which were felt in the immediate vicinity of the epicentres, and were responsible for minor damage to goods and a few weak structures. A magnitude 5. Other shocks of magnitude 5 or more occurred near Pahiatua on February 14, and in Fiordland on 15 September.
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On 23 November small shocks were reported from Timaru and Oamaru. By arrangement with the administrations concerned the Service performs similar functions for British territories in the Pacific. Weather reports for use in forecasting are made at about places within New Zealand and 50 in Pacific islands and collected by telegraph and radio, along with measurements of winds at upper levels made at nine radio wind stations and of temperatures made at eight radiosonde stations. Daily observations are made for climatological purposes at about places in New Zealand and 80 in the islands.
Rainfall measurements are made at a total of about 2, places within New Zealand and outside the country. The weather pattern from day to day is dominated by a succession of anticyclones, separated by troughs of low pressure, which pass more or less regularly from west to east across the Australia - Tasman Sea - New Zealand area and beyond. In this region there is no semi-permanent anti-cyclone such as those found in similar latitudes over the Indian Ocean and eastern Pacific Ocean respectively.
The troughs normally have a northwest to southwest orientation and are associated with deep depressions centred far to the south. A typical weather sequence commences with a low-pressure trough approaching from the west. Freshening northwesterly winds prevail with increasing cloud, followed by rain for a period during which winds may reach gale force.
The passage of the trough, with its associated cold front, is accompanied by a change to cold southwesterly or southerly winds and showery weather, occasionally with some hail and thunder. Barometers then rise with the approach of the next anticyclone from the west. Winds moderate and fair weather prevails for a few days as the anticyclone moves across the country.
While the sequence just described is very common the situation is frequently much more complex. The troughs are very unstable systems where depressions readily form, some of which develop into vigorous storms that may pass over New Zealand at any time of the year. Occasionally in summer a cyclonic storm of tropical origin passes over or near New Zealand accompanied by gales and heavy rain affecting mainly northern and eastern districts of the North Island.
The anticyclones vary in size, intensity, and rate of movement. Their centres, on the average, follow a track across the North Island but individual centres may pass either north or south of the country, the more northerly tracks being favoured in spring and the southerly tracks in autumn. At times when little development occurs within the troughs the anticyclones follow each other at intervals of about days.
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The other main factors which influence the climate of New Zealand are, first, its position in the midst of a vast ocean, and second, the shape and topography of the country itself. Australia, the nearest continent, is 1, miles to the west and Antarctica is 1, miles to the south. Hot air masses from the interior of Australia in summer, or freezing air masses from the Antarctic, which occasionally reach New Zealand, retain little of their original character after their long ocean passage.
Thus, there is an absence of extreme variations of temperature. On the other hand, since abundant supplies of moisture are supplied by evaporation from the oceans, and depressions are frequent and vigorous, the average precipitation is high. The chain of high mountains, which extends from south-west to north-east through the length of the country, rises as a formidable barrier in the path of the prevailing westerly winds.
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The effect is to produce much sharper climatic contrasts from west to east than in the north-south direction. In some inland areas of the South Island just east of the mountains the climate is distinctly continental in character, despite the fact that no part of New Zealand is more than 80 miles from the sea. Winds —Winds from a westerly quarter prevail in all seasons, with a general tendency to increase in strength from north to south.
However, considerable local modifications to the general air flow occur during its passage across the mountainous terrain. Approaching the main ranges the flow from the west turns towards the north-east and on descending on the eastern side swings towards the south-east. This results in an increased number of south-westerlies in Westland and a predominance of north-westerlies in inland districts of Otago and Canterbury, where strong gales from this quarter occur at times in the late spring and summer.
Daytime sea breezes usually extend from the coast inland for 20 miles or more during periods of settled weather in summer. On the Canterbury coast the wind comes most frequently from the north-east, partly because there is a persistent sea breeze from this quarter, but south of Dunedin south-westerlies predominate. Cook Strait, the only substantial gap in the main mountain chain, acts as a natural funnel for the air flow and is a particularly windy locality afflicted by gales from the south-east as well as the north-west.
North of Taranaki the general air flow is more from the south-west, and there is a noticeable reduction in windiness in the summer. An indication of the variation in the frequency of strong winds from summer to winter, and in different parts of the country, is given in the next table. These were all obtained by the use of Dines pressure-tube anemometers at well exposed sites.
Rainfall —The distribution of rainfall is mainly controlled by mountain features, and the highest rainfalls occur where the mountains are exposed to the direct sweep of the westerly and north-westerly winds.
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The mean annual rainfall see map ranges from as little as mm in a small area of Central Otago to over mm in the Southern Alps. The average for the whole country is high, but for the greater part it lies between and mm, a range regarded as favourable for plant growth in the temperate zone. The only areas with under mm are found in the South Island, to the east of the main ranges. In the North Island, the driest areas are central and southern Hawke's Bay, Wairarapa, and Manawatu where the average rainfall is mm a year. Of the remainder, much valuable farm land, chiefly in northern Taranaki and Northland, has upwards of mm.
Over a sizeable area of both Islands rainfall exceeds mm a year but, with the exception of Westland, this is mountainous and unoccupied, much of it being forest covered. For a large part of the country the rainfall is spread evenly through the year.