Burma Weather July

Weather in July

Burmese weather in July is the peak of the monsoon season, with heavy, almost daily rains for most of the country. Not many foreign tourists in May, July and September. Cyclone KOMEN at the end of July. Weather Forecast for MYANMAR / Burma. lndia, even if they are all influenced by similar weather systems.

July average weather in Hpa-an, Myanmar (Burma)

The high temperature every night is around 83°F, seldom below 80°F or above 87°F. The lowest temperature every days is around 77°F, seldom below 75°F or above 79°F. On April 12, the warmest of the year, Hpa temperature is between 78°F and 95°F, while on January 3, the colder part of the year, it is between 64°F and 85°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 (4,878 leagues away) is the farthest strange place with temperature most similar to that of Hpa-an (see comparison). July in Hpa - a substantially steady blanket of clouds, with the percent of the period when the skies are covered or mostly overcast being around 92% throughout the year. Most clear days of the months are July 25th, with clear, mostly clear or partially crowded weather 9% of the year.

At Hpa-an, the probability of a rainy morning increases during July, beginning at 74% and ending at 79%. By comparison, the highest probability of a rainy diurnal is 80% on August 4 and the lowliest 1% on January 27.

Mean 31-day moving precipitation in July in Hpa-an is rising very quickly, beginning the months at 11. 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 Hpa-an days 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).

Hpa-an's earlyest dawn of the months is 5:29 am on July 1 and the last dawn is 9 mins later at 5:39 am on July 31. Last sundown is on July 6th at 6:37 pm and first sundown is 5 min early at 6:32 pm on July 31st.

Hpa-an will not keep to daylight savings in 2018. On June 21, the longest of the year, the sun will rise at 5:27 am and set 13 hrs, 8 mins later at 6:35 pm, while on December 21, the shorter days of the year, the sun will rise at 6:23 am and set 11 hrs, 7 mins later at 5:31 pm.

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. In Hpa-an, the probability that a certain date will be humid is basically stable in July and remains at 100% throughout.

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. All over July the mean windspeed in Hpa-an per hours is substantially stable and remains within 0. 1 mph of 7. 5 mph.

Note on July 28, the most windy of the year, the mean windspeed is 7. 6 mph, while on February 2, the quietest of the year, the mean windspeed is 3. 5 mph. Maximum mean windspeed during July is 7. 6 mph on July 28th.

Averages of the mean windspeeds per hour (dark grey line), with 25 to 75 and 10 to 90 centilbands. Proportion of Hour in which the mean windspeed comes from each of the four main winds (North, east, southwest and west), 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). The Hpa-an is situated near a large river (e.g. oceans, seas or large lakes). In this section, the mean shallow waters are reported.

In Hpa-an, the mean sea level in July is substantially stable and remains around 83°F throughout. 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).

Hpa-an's year round weather is so mild that it is not very informative to talk about the vegetation period in this sense. 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. Hpa-an cumulative growth rates increase sharply in July, rising by 886°F during the course of the months from 5,407°F to 6,293°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.

In Hpa-an, the mean short-wave short-wave sun power averaged per day is substantially stable during July and remains within 0. 1 kilowatt hour out of 4. 4 kilowatt hours. 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 Hpa-an 16.

Hpa-an's 2 mile landscape contains only moderate differences in altitude, with a peak alteration of 361 ft and an mean altitude of 47 ft above sealevel. There are only slight differences in altitude within 10 mile ('2,057 feet). There are great differences in altitude within 50 mile ('6,788 feet).

Hpa-an is 2 mile farmland (43%), 25% hydrological (25%) and tree (16%), 10 mile farmland (54%) and tree (23%) and 50 mile farmland (29%) and tree (24%) area. The following is a one-year weather forecast for Hpa using a statistically accurate annual weather forecast from January 1, 1980 to December 31, 2016, using historic weather data and models.

We have 2 weather wards close enough to help estimate the temperatures and condensation points in Hpa-an. Recordings for each ward are adjusted for the altitude differential between that ward and Hpa-an according to the International Standard Atmosphere and for the rel. variation present in the MERRA-2 space age re-analysis between the two sorts.

Hpa-an is calculated as the weight of each item, the weight being in proportion to the inversion of the Hpa-an to a given one. 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. The weather 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.

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