Forecast Auckland new Zealand

. The minimum temperature increases by 3°F, from 49°F to 52°F, seldom below 42°F or above 57°F. On February 6th, the warmest of the year, Auckland' s temperature is usually between 63°F and 74°F, while on July 15th, the colder part of the year, it is between 47°F and 57°F.

Mean maximum day (red line) and minimum day (blue line) with 25 to 75 and 10 to 90 percent ribbons. Thin dashed line is the corresponding mean observed heat. In the following illustration you can see a concise characterisation of the mean annual weather for the September period.

Horiz. The horiz. axle is the tag, the vertic. axle is the hours of the days, and the colour is the mean temper. for that hours and that days. Mean hrs temp, colour encoded in bands: chilled < 15°F < freezed < 32°F < very chilled < 45°F < chilled < 55°F < chilled < 65°F < comfortably < 75°F < warmed < 85°F < heated < 95°F < stewed.

Portugal (12,063 leagues away) is the farthest strange place with the most similar to Auckland. September in Auckland is dominated by a steady clouding, with the proportion of the period in which the skies are covered or very clear being around 41% throughout the whole months. Most clear September 1st is the most clear date of the months, with clear, mostly clear or partially cloudily weather 61% of the year.

The likelihood of a rainy morning in Auckland during September is largely stable at around 31%. The highest probability of a rainy morning on July 18th is 37%, the lowliest on January 28th is 17%. In order to show the variations within the months and not only the sum of the months, we show the precipitation that has collected over a 31 days cycle, which revolves around each one.

In Auckland, the statistic 31 era gliding precipitation during September decrease gradually and point the time period at 3. 0 linear unit if it seldom tops 5. Inch or drops below 1. 1 inch, ending the months at 2. 7 inch if it seldom rises above 4. Mean precipitation (solid line) collected over a moving interval of 31 days, centred on the relevant date, with 25 to 75 and 10 to 90.

Thin dashed line is the corresponding mean fluid equivalents of snow. In the course of September, the length of the days in Auckland rises dramatically. Between the beginning of the week and the end of the week, the length of the days is increased by 1 hr, 7 min, which means an approximate ascent of 2 min, 18 sec and a week ascent of 16 min, 7 sec.

September 1st is the briefest date of the months with 11 hrs, 18 min and the longest date is September 30th with 12 hrs, 24 min. of sunlight. This is the number of times the sun is seen (black line). Auckland' s early morning is 6:00 am on September 29 and the latest is 59 min later at 6:59 am on September 30.

Early sundown is 6:00 pm on September 1st and the latest sundown is 1h, 23min later at 7:23 pm on September 30th. Summertide ( "summertime") begins on September 30, 2018 at 3:00 am and postpones the rising and setting of the sun to one second. On December 21, the longest of the year, the sun comes up at 5:57 am and goes down 14 hrs, 42 mins later at 8:39 pm, while it comes up on June 21, the shorter part of the year, at 7:33 am and 9 hrs, 38 mins later, at 5:11 pm.

A sunny working days in September. Contrary to the typical fluctuation between nights and days, the tendency is for the condensation point to vary more gradually so that the temperatures can decrease at nights, while a sultry and humid full moon is followed by a sultry one. In Auckland, the likelihood of a particular date becoming sultry in September is largely stable at around 0%.

In this section the mean value of the windvector (speed and direction) at a height of 10 metres above the floor is discussed. Winds at a given place are strongly influenced by geographic conditions and other variables, and the current windspeed and heading varies more than the hoursly mean. Auckland' s annual windspeed rises from 14 in September.

up to 15 mph. six mph during the course of the months. On October 3, the most windy of the year, the mean windspeed is 15. averages 7 mph, while on February 8th, the quietest days of the year, the mean windspeed is 12 per da.

Three-mile per hr. In September the slowest mean daytime windspeed is 14. September 2nd, three mile per hr. Averages of the mean windspeeds per hour (dark grey line), with 25 to 75 and 10 to 90 centilbands. Proportion of hrs in which the mean windspeed comes from each of the four main winds (North, east, southwest and west), except for hrs in which the mean windspeed is less than 1mbar.

Slightly toned areas at the borders are the percent of the number of hrs passed in the implicit intersections (northeast, south east, south west and northwest). The Auckland is situated near a large river (e.g. oceans, seas or large lakes). In this section, the mean shallow waters are reported.

Auckland' s mean sea level remains largely stable throughout September at between 1°F and 58°F. Diurnal mean diurnal watermarking ( "purple line"), with 25 to 75 and 10 to 90 centils. Vegetation cycle definition varies worldwide, but for the purpose of this document we have defined it as the longest uninterrupted non-icing cycle ( 32°F) in the year (the northern hemisphere or from July 1 to June 30 in the southern hemisphere).

Auckland' s year round climate is so mild that it is not very informative to talk about the vegetation period. However, as an example of the way in which the year' s average annual average annual average body heat is distributed, we have included the following graph. Proportion of cooling period in different ranges: cooling < 15°F < freeze < 32°F < very low < 45°F < low < low < 55°F < low < low < 65°F < pleasant < 75°F < high < 85°F < high < 95°F < glowing.

Rising degrees day is a measurement of the annual storage of thermal energy used to forecast the evolution of plants and animals and is measured as the thermal integrity above a basic level, where surpluses above a peak level are discarded. Auckland' s cumulative growth rate is rising steadily in September, rising 158°F over the course of the months from 205°F to 363°F.

In the course of September, the weighted number of growth dates cumulated to 25 to 75 and 10 to 90. In this section, all the short-wave sunlight entering the earth's atmosphere every morning reaches the earth's crust over a large area, taking full consideration of seasons, the height of the sun above the horizontal plane and its absorbance by the sun's ultra-sound.

Auckland' s short-wave short-wave annual power consumption increases by 1.3 kilowatt-hours in September from 3.7 kilowatt-hours to 4.9 kilowatt-hours during the course of the year. Averages the short-wave short-wave sun power per day that reaches the floor per m2 (orange line), with 25 to 75 and 10 to 90 percent band.

The geographic co-ordinates of Auckland for the purpose of this review are -36. 867 degrees of latitude, 174. Auckland' s 2 mile landscape contains significant differences in altitude, with a peak alteration of 607 ft and an mean altitude of 182 ft. Auckland' s area is coated with man-made surface (82%) within 2 mile, within 10 mile it is coated with irrigation (36%) and grasslands (26%) and within 50 mile it is coated with irrigation (66%) and tree (17%).

Auckland' s characteristic year round forecast, depicting Auckland' s characteristic meteorological conditions, using historic hours and models from January 1, 1980 to December 31, 2016. There' s only one meteorological data point in our database, Auckland International Airport, which can be used as a protocol for Auckland's historic temperatures and condensation data.

Located 16 kilometres from Auckland, nearer than our 150 kilometre limit, this location is considered sufficiently close to be our main point of reference for recording temperatures and deaths. Meteorological data are adjusted for the altitude differences between the meteorological observatory and Auckland according to the International Standard Atmosphere and for the changes that have occurred in the re-analysis of the MERRA-2 satellites between the two sites.

The rest of the meteorology, which includes clouds, rainfall, wind velocity and orientation, and sun flow, is taken from NASA's MERRA-2 Modern-Era Retrospective Analysis. The re-analysis will combine a multitude of large-area readings in a state-of-the-art worldwide metrological modell to recreate the hours' histories of the earth's climate on a 50-kilometer-raster.