Nay Pyi Taw WeatherWeather in Nay Pyi Taw
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Weather in Nay Pyi Taw, Myanmar (Burma), average weather throughout the year
During the year, the typical annual temperatures vary between 61°F and 103°F and seldom fall below 56°F or above 108°F. The best seasons to come to Nay Pyi Taw for warm weather activity are from the end of February to mid-April and from early November to early December.
It is a 7-month period, from 17 March to 9 May, with an elevated mean daytime heat of over 100°F. April 14th is the warmest of the year with an averaging high of 103°F and a low of 78°F. Zero month, from 1 December to 1 February, with an maximum daytime mean temp below 92°F.
January 24 is the coolest date of the year with an annual low of 61°F and a high of 91°F. Mean maximum and minimum days (red line) with 25 to 75 th and 10 to 90 th centils. Thin dashed line is the corresponding mean observed heat.
In the following illustration, a concise characterisation of the whole year of annual mean surface water usage is shown. It is the date of the year, the time of the year is the horizon of the year, and the colour is the mean price for that time. 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.
At Nay Pyi Taw, the mean cloud cover varies greatly throughout the year. nine month and ends around April 26. By 21 February, the brightest of the year, the skies are clear, mostly clear or partially overcast 82% of the year, and mostly or heavily or heavily clouded 18% of the year.
Most of the year starts around April 26th and takes 6 years. August 4, the most cloudy days of the year, the skies are clear or 91% and 9% clear, mostly clear or particlar. Proportion of total elapsed cloudband period categorised by the percent of clear < 20% < mostly clear < 40% < partially cloudily < 60% < mostly cloudily < 80% < haze.
Smallest chances of a rainy evening is 1% on January 31st. Proportion of the number of times different kinds of rains are seen, except for amounts of traces: rains alone, snows alone and combined (rain and snows falling on the same day). 3- month, from 14 April to 22 November, with 31 consecutive rains of at least 0.5-inch.
Most of the rains during the 31 era centred around July 31, with an statistic whole group of 2. 8in. Seven month, from November 22nd to April 14th. Little rains fall around February 12, with an overall collection of 0. 1in. on the whole. Mean precipitation (solid line) collected over a 31-day moving interval, centred on the relevant date, 25 to 75 and 10 to 90.
Thin dashed line is the corresponding mean fluid equivalents of snow. Early morning is June 6th at 5:25 am and the latest is 1 hours, 17 min later at 6:42 am on January 18th. Nay Pyi Taw does not observe daylight savings in 2018. 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.
The Nay Pyi Taw experience extremely strong variations in air moisture. from 9 April to 1 December, when in at least 25% of cases comforts are humid, distressing or atrocious. On the most humid days of the year is August 15th, with the most humid weather 100% of the year.
On the least turgid date of the year is 26 January, when the muggiest weather is largely unknown. Proportion of the amount of time passed at different moisture-comforts grades categorised by the following factors: dehydration < 55°F < convenient < 60°F < humid < 65°F < humid < 70°F < depressing < 75°F < drought.
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. Nay Pyi Taw's mean windspeed per hour is strongly seasonally-dependant.
A 3-month period, from 18 May to 29 August, with windspeeds averaging more than 6.1 mph. Most windy is June 25th, with an annual windspeed of 8.5 mph. During the quieter season it takes 8 years. Most quiet of the year is November 8th, with an annual windspeed of 3. 8 mph.
Averages of the mean windspeeds per hour (dark grey line), with 25 to 75 and 10 to 90 centilbands. Nay Pyi Taw's prevailing mean winds per hour vary throughout the year. Winds come most often from the southern for 1. 7 week, from 4 January to 16 January and for 7week.
1st month, from 4th May to 6th December, with a top value of 86% on 2nd July The winds come most frequently from the western hemisphere for 3rd quarter. Six-month period, from 16 January to 4 May, with a record 58% on 7 April. Winds come most often from the eastern part for 4.
1st week, from 6 December to 4 January, with a top value of 32% on 1 January. Proportion of Hour in which the mean windspeed comes from each of the four main winds (North, East, S and W ), 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, south east, south west and northwest). In order to characterise how comfortable the weather in Nay Pyi Taw is all year round, we calculate two trip values. Tourist evaluation favours clear, rainy weather with a temperature between 65°F and 80°F.
On the basis of this result, the best season to go to Nay Pyi Taw for general open-air touristic activity is from early December to early March, with a top value in the first weeks of January. Touristic value (filled area) and its components: the value of temperatures (red line), the value of clouds (blue line) and the value of rainfall (green line).
Swimming pools provide clear, rainy weather with a temperature between 75°F and 90°F. On the basis of this result, the best time of the year to go to Nay Pyi Taw for warm weather activity is from the end of February to mid-April and from early November to early December, with a record in the third weeks of March.
Strand/bathing value (filled area) and its components: value of water temperatures (red line), value of clouds (blue line) and value of rainfall (green line). Separate values for temperatures, clouds and overall rainfall are calculated for each lesson between 8:00 and 21:00 on each daily in the analytical time frame (1980 to 2016).
These values are summarized into a singular total number of points per hour, which is then aggregate into numbers of day, meand ged and flattened over all years in the time frame for each year. The cloudflood value is 10 for fully clear sky, which falls linear to 9 for mostly clear sky and 1 for completely cloudy sky.
The rainfall value is 10 for no rainfall, falls linear to 9 for lane rainfall and to 0.04in or more. The tourist price is 0 for felt values below 50°F, increases linear to 9 for 65°F, to 10 for 75°F, falls linear to 9 for 80°F and to 1 for 90°F or warmer.
We have a beach/pool temp readout of 0 for sensed temp below 65°F, rises linear to 9 for 75°F, 10 for 82°F, falls linear to 9 for 90°F and 1 for 100°F or warmer. 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.
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 level, where surpluses above a maximal level are discarded.
During the year, the annual growth rate is 25 th to 75 th and 10 th to 90 th. 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.
Short-wave sunlight is required on avarage days throughout the year. Lighter periods of the year last 2. 1 month, from 24 February to 28 April, with an annual mean short-wave power input per sq. metre above 6. Daylight is the 1st of April with an annual mean of 6.7 kilowatt-hours.
for 5 month, from 22 June to 8 January, with an annual short-wave power output per m² below 5.2 kilowatt hours. On August 5th, the darkiest date of the year is 4.8 kilowatt-hours on averages. Averages the short-wave short-wave sun power per m² per night that reaches the floor (orange line), with 25 to 75 and 10 to 90 percent band.
Nay Pyi Taw's 2 mile landscape contains only moderate differences in altitude, with a peak alteration of 161 ft and an mean altitude of 398 ft aboveseas. The following article shows the weather in Nay Pyi Taw, on the basis of a statistic study of historic weather records per hour and models from January 1, 1980 to December 31, 2016.
There' s only one weather data point in our Nay Pyi Taw database, Sanam Bin Mae Hong Son, which can be used as a protocol for the historic Nay Pyi Taw temperatures and dots. 200 kilometres from Nay Pyi Taw, further than our 150 kilometre limit, this location is considered inadequately situated to be our main point of reference for recording temperatures and depression.
The MERRA-2' s mass is 50% and that of the weather forecast is 50%. The other weather information, 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 weather forecasting tool to recreate the hours' weather histories around the globe on a 50-kilometer raster.
The name, location and timezones of places and some airfields are taken from the GeoNames Geographical Database. Timezones for airfields and weather station are provided by AskGeo.com. Meteorological information is susceptible to faults, failures and other faults. are ( (1) computer modelling, which may have model-based faults, (2) are roughly scanned on a 50 km raster and are therefore not able to recreate the microclimate fluctuations locally, and (3) have particular difficulties with the weather in some coastlines, especially small isles.
Please also note that our trip values are only as good as the underlying information, that weather at a particular place and at a particular point in times is unforeseeable and fluctuating, and that the values defined reflect a particular category of preference that may not match that of a particular readership.