Temperature in Pyin Oo Lwin

Pyin Oo Lwin temperature

July average weather in Pyin Oo Lwin, Myanmar (Burma) The high temperature every night is around 87°F, seldom below 81°F or above 92°F. The minimum temperature every night is around 69°F, seldom below 66°F or above 72°F. On April 19, the warmest of the year, Pyin Oo Lwin usually has a temperature between 67°F and 92°F, while on January 15, the colder part of the year, the temperature ranges between 47°F and 77°F.

Mean maximum temperature (red line) and minimum temperature (blue line) with 25 to 75 and 10 to 90 percent ribbons. Thin dashed line is the corresponding mean temperature read. In the following illustration, a concise characterisation of the mean temperature per hour for the month of July is shown.

Horiz. The horiz. axle is the tag, the vertic. axle is the hours of the days, and the colour is the mean temperature for that hours and that days. Mean temperature per hours, color-coded in strips: chilled < 15°F < freezed < 32°F < very chilled < 45°F < chilled < 55°F < chilled < 65°F < convenient < 75°F < warmed < 85°F < heated < 95°F < stewed.

Tsumeb, Namibia (6,038 mile away ); Hwange, Zimbabwe (5,495 miles); and Chiredzi, Zimbabwe (5,290 miles) are the most distant overseas locations with similarities to Pyin Oo Lwin (see comparison). July in Pyin Oo Lwin has a substantially stable blanket of clouds, with the proportion of the period in which the skies are covered or heavily clouded being around 89% throughout the whole months.

On 23 July, the highest probability that it is covered or heavily clouded is 90%. Most clear days of the months are July 1st, with clear, mostly clear or partially crowded weather 13% of the year. On 23 July, the most cloudy of the year, the probability of clouds is 90%, while on 23 February, the brightest of the year, the probability of a clear, mostly clear or partially cloud-covered sky is 87%.

At Pyin Oo Lwin, the probability of a rainy morning increases progressively during July, from 6% to 8%. By comparison: The highest probability of a rainy morning on 3 June is 17%, the lowliest on 22 February 1%.

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. Some 31-days moving precipitation during July in Pyin Oo Lwin is substantially stable and remains approximately 0. 3-inch throughout, seldom surpassing 1.

Minimum mean cumulation of 31 days is 0.3 inch on July 12. 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 July the length of the days in Pyin Oo Lwin slowly diminishes. Between the beginning of the week and the end of the week, the length of the days is reduced by 19 min, which means an annual mean of 37 seconds and a 4-minute and 20-second reduction per week.

July 31 is the briefest date of the months with 13 hrs, 9 min and the longest date is July 1 with 13 hrs, 28 min. of sunlight. This is the number of times the sun is seen (black line). Pyin Oo Lwin's earlyest dawn of the months is 5:24 am on July 1 and the latest dawn is 12 min later at 5:35 am on July 31.

Last sundown is at 6:51 pm on July 4th and first sundown at 6:45 pm on July 31st. Summer season will not be respected in Pyin Oo Lwin in 2018. On June 21, the longest of the year, the sun will rise at 5:21 am and set 13 hrs, 29 mins later at 6:50 pm, while on December 21, the shorter days of the year, the sun will rise at 6:38 am and set 10 hrs, 47 mins later at 5:25 pm.

A sunny peninsula in July. Contrary to the temperature, which usually fluctuates greatly between the nights and days, the temperature tends to vary more gradually so that the temperature can decrease at nights, while a sultry and humid full moon is followed by a sultry one. In July, the probability of a particular date becoming sultry in Pyin Oo Lwin is substantially stable at 1% of 68%.

By comparison, on June 22, the sultriest of the year, there are more sultry weather 70% of the year, while on January 1, the sultriest of the year, there are more sultry weather 0% of the year. 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. Mean windspeed in Pyin Oo Lwin drops during July from 8. 9 mph to 7. 6 mph above the course of the mont.

On June 29, the most windy of the year, the windspeed is 8. 9 mph, while on October 14, the quietest days of the year, the windspeed is 4. 2 mph. Maximum mean windspeed in July is 8.9 mph on July 3rd The mean windspeeds per hours (dark grey line), with 25 to 75 th and 10 to 90 th percentiles are averaged.

Proportion of Hour in which the mean windspeed comes from each of the four main winds (North, east, southerly and westerly), except when the mean windspeed is less than 1ph. Slightly toned areas at the borders are the percent of the number of hrs passed in the implicit intersections (northeast, sutheast, southwest und northwest).

Vegetation cycle definition varies worldwide, but for the purpose of this document we have defined it as the longest uninterrupted non-icing temperature cycle ( 32°F) in the year (the northern hemisphere or from July 1 to June 30 in the southern hemisphere).

The temperature in Pyin Oo Lwin is so mild all year round that it is not quite clear to talk about the vegetation period. However, as an example of the temperature distributions over the year, we have included the following graph. Proportion of cooling period in different temperature ranges: cooling < 15°F < freeze < 32°F < very cooling < 45°F < cooling < 55°F < cooling < 65°F < pleasant < 75°F < heating < 85°F < heating < 95°F < glowing.

This is the probability in percent that a certain date is within the vegetation period. Increasing degrees are a measurement of the annual storage of thermal energy, which is used to forecast the evolution of plants and animals and is measured as the thermal integrity above a basic temperature, where surpluses above a maximal temperature are discarded.

Averages of cumulative growth in Pyin Oo Lwin are rising at a rapid pace in July, rising by 806°F during the course of the months from 4,003°F to 4,810°F. In the course of July, the weighted growth rate cumulated at 25 to 75 and 10 to 90. In this section, the entire 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.

In Pyin Oo Lwin, the short-wave short-wave sun's annual power output is substantially stable in July and remains within 0.2 kilowatt-hours out of 5. 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 Pyin Oo Lwin for the purpose of this document are 22.

Geographical location within 2 mile of Pyin Oo Lwin contains significant altitude differences, with a peak alteration of 515 ft and an mean altitude above sealevel of 3,536 ft. There are considerable differences in altitude within 10 mile ('4,029 feet). There are also extremely high differences within 50 Mile (.994 feet).

This area is within 2 mile of Pyin Oo Lwin clouded by farmland (68%) and tree (15%), within 10 mile of farmland (37%) and bushes (33%) and within 50 mile of farmland (34%) and bushes (29%). The following article shows the average Pyin Oo Lwin year round meteorological conditions, using a statistic study of historic hoursly meteorological records and models from January 1, 1980 to December 31, 2016.

The Pyin Oo Lwin is more than 200 kilometres from the next dependable meteorology centre, so the weather-related information on this page is entirely from NASA's MERRA-2 time. 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.

Temperature and condensation point estimations are adjusted by the differential between the MERRA-2 grating height and the height of Pyin Oo Lwin according to International Standard Atmosphere. Please also note that our trip values are only as good as the underlying information, that at a given place and at a given point in due course meteorological events are unforeseeable and fluctuating, and that the values defined reflect a particular category of preference that may not match that of a particular readership.

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