Yangon Weather JulyWeather in July
July average weather in Yangon, Myanmar (Burma)
The high temperature every night is around 85°F, seldom below 80°F or above 89°F. The lowest temperature every days is around 77°F, seldom below 75°F or above 79°F. On April 12, the warmest days of the year, Yangon's temperature is usually between 78°F and 97°F, while on January 10, the colder days of the year, it is between 67°F and 88°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, a concise characterisation of the mean annual weather conditions 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 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.
Nkove, Tanzania (4,782 mile away ) is the faraway strange place with temperature most similar to Yangon (see comparison). July in Yangon is mostly constantly cloudily, with the average period in which the skies are covered or mostly cloudily being around 92% throughout the year. Most clear days of the months are July 26th, with clear, mostly clear or partially crowded weather 8% of the usual rain.
At Yangon, the probability of a rainy morning increases progressively during July, from 53% to 55%. The highest probability of a rainy morning is 55% on August 7th, the lowliest 1% on January 26th.
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. Averaging 31-days moving precipitation during July in Yangon is rising fast, beginning the months at 7. 6-inch, when it seldom rises above 16.
6 inch and finishes the months at 9. 1 inch if it seldom rises above 21. Highest 31-days mean cumulation is 9. 1 inch on July 31. 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 Yangon River is largely the same. July 31 is the briefest date of the months with 12 hrs, 53 min and the longest date is July 1 with 13 hrs, 7 min. of sunlight.
This is the number of times the sun is seen (black line). Yangon's earlyest dawn of the months is 5:35 am on July 1 and the latest dawn is 9 mins later at 5:45 am on July 31. Last sundown is on July 7th at 6:42 pm and first sundown is 5 min early at 6:38 pm on July 31st.
Summer break in Yangon in 2018. On June 21, the longest of the year, the sun will rise at 5:33am and set 13hrs, 8min later at 6:41pm, while on December 21, the shorter part of the year, it will rise at 6:29am and set 11hrs, 8min later at 5:37pm.
A sunny peninsula in July. 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. Yangon's likelihood of a particular date becoming sultry in July is largely stable and remains around 100% throughout 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. Yangon's mean windspeed per hours in July is substantially stable and remains within 0.2 mph of 10.
On June 25, the most windy of the year, the mean windspeed is 10. on the quietest days of the year, the mean windspeed per minute is 5. 8 mph. Averages of the mean windspeeds per hours (dark grey line), with 25 to 75 and 10 to 90 percent band.
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).
The Yangon is near a large river (e.g. oceans, seas or large lakes). In this section, the mean shallow waters are reported. Yangon's mean freshwater temperatures are largely stable in July and remain around 83°F throughout the year. 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 temperature cycle ( 32°F) in the year (the northern hemisphere or from July 1 to June 30 in the southern hemisphere).
Yangon's year round weather 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. Yangon's cumulative growth rate is rising at a rapid pace in July, rising by 896°F during the course of the months from 5,490°F to 6,386°F.
In the course of July, the weighted growth rate cumulated at 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.
Yangon's short-wave short-wave mean day-to-day sun power is substantially stable in July and remains within 0.1 kilowatt-hours of 4.1 kilowatt-hours. In July, the minimum mean dayly sun power is 4.0 kilowatt hours on 28 July. 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 Yangon for the purpose of this review are 16. Yangon's 2 mile landscape contains only moderate differences in altitude, with a peak alteration of 213 ft and an mean altitude of 78 ft above sealevel. Yangon is 2 mile farmland (63%) and arable (19%), 10 mile farmland (60%) and 14% farmland (14%) and 50 mile farmland (52%) and 30% farmland (30%) high.
Weather in Yangon throughout the year, on the basis of a statistically accurate annual weather forecast and models from January 1, 1980 to December 31, 2016. There' s only one weather data point in our database, Yangon International Airport, which can be used as a protocol for Yangon's historic temperatures and dewpoint.
Located 12 kilometres from Yangon, 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 base and Yangon according to the International Standard Atmosphere and for the changes in the MERRA-2 satellites between the two sites during the re-analysis.
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.
Timezones for airports 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.