The release of the monthly weather forecast for Jordan for January 2021, with full details inside

Jordan | January 2021: The month begins with a warm, stable and dry climate followed by the "return of winter" approaching the middle of the month

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The most prominent expected weather phenomena:

General situation:

1. The month of January begins with dry weather, warm spell, and stable weather.

2. A radical change is expected in the weather system, approaching the middle of the month, with the return of the high chances of rain and cold.

3. Low air that may be classified as advanced degrees in the third week, and normal winter conditions in the fourth week.

4. The decrease in the need to use heating methods in the first period of the month, and the increase in the need for intensive irrigation of crops in the same period for agricultural areas.

5. The break of the eastern winds is expected after the tenth of the month.

Expected weather systems:

30 day daily forecast | Rainfall days and temperature behavior:

Temperature deviation from the general monthly averages:

Rainfall deviation from the general monthly averages:

Detailed weather condition:

First week (1-7) January 2021:

• Rain
  
  • Less than (average dry).
• Temperatures
  
  • Warmer than the rates (wave of warmth).
• Torrents opportunity
  
  • There is no.
• Snow opportunity
  
  • There is no.
• Description of air systems
  
  • Pan Levant regions and Jordan are affected by a wave of warmth caused by the flow of warm air currents in the middle and upper layers of the atmosphere coming from the Sahara and stable atmosphere , so expect that the temperatures rise, especially at the end of an extraordinary week from the usual rates for this time of the year amid Stable in all regions and tends to heat in the Jordan Valley, Dead Sea and Aqaba regions at the weekend.

Second week (8-14) January 2021:

• Rain
  
  • To less than about rates.
• Temperatures
  
  • About to warmer than the rates.
• Torrents opportunity
  
  • Low.
• Snow opportunity
  
  • Low.
• Description of air systems
  
  • Jordan and the Levant continue to be affected by the same warm air currents, with temperatures warmer than normal and the chances of rain weak. As the end of this week approaches, indications are increasing that the region will be affected by an extension of an air depression that will lead to a return to temperatures and an increase in the chances of rain in northern and central Jordan, God willing. A break of the eastern winds is expected after the tenth of the month.

Third week (15-21) January 2021:

• Rain
  
  • Higher rates.
• Temperatures
  
  • About to colder than rates.
• Torrents opportunity
  
  • Medium.
• Snow opportunity
  
  • Medium chance on medium mountains rise in the Levant.
• Description of air systems
  
  • Is expected to be a radical change in the system so that air rushes to a low area Joey believes he will sort of advanced degrees and brings with abundant amounts of rain , God willing, and as temperatures will reduce dramatically and become a tangible atmosphere of the beginnings of a much colder month. There is an average chance that the medium-rise mountains in the Levant will be exposed to snowfall, God willing.

The fourth week and the last days of the month (22-31) January 2021:

• Rain
  
  • About rates.
• Temperatures
  
  • About the rates.
• Torrents opportunity
  
  • Low.
• Snow opportunity
  
  • Low.
• Description of air systems
  
  • Indications indicate that the eastern and southeastern parts of the European continent are increasingly affected by strong depressions, some of which may extend to the central and eastern Mediterranean regions, including the Jordan and the Levant, so that temperatures and rains are expected to be recorded around their rates and perhaps higher, especially in Lebanon. And Syria.

Climate situation (for professionals and interested parties):

Most global climate monitoring centers monitor the occurrence of what is called Sudden stratospheric warming, which is occurring at an altitude of approximately 30 km above the earth's surface, specifically above the Arctic Circle. This phenomenon, which recurs every several years and occurs in winters in the northern hemisphere of the globe, has a great impact on changing the weather patterns prevailing in the rest of the winter in the northern hemisphere because of its impact on the so-called polar vortex (Polar Vortex) And from which the winter depressions branch out, with both rainy and snowy parts, on the continents of the North of the Earth. This polar vortex is coherent in its natural position over the North Pole and has branches in several regions and is responsible, after the will of God, for the development of deep atmospheric depressions.

What happens as a result of the sudden stratospheric warming sometimes directly affects this polar vortex and may lead to its splitting into two, depending on where this warming occurred over the Arctic Circle. This event, which is believed to have already started at the time of writing (early January 2021), is believed to be one of the times this warming will be strong enough to split this polar vortex in two and in such a way that there will be a large accumulation of extreme polar cold in the northwest The continent of Asia, the pan-European continent, where a strong polar current is expected to flow to the west of the European continent before it merges with other intense polar currents in the east of the European continent and accumulates there for a period of time. It is important to mention that this happens because of the same phenomenon represented by sudden stratospheric warming, and despite its occurrence at high altitudes above the surface of the earth in the atmosphere, its impact reaches altitudes close to the surface of the earth, especially in those layers that control the weather and the shape of atmospheric patterns. , So that it results in the escape of currents and polar masses away from their original home, which is the North Pole, to be distributed randomly in the northern hemisphere continents, which also may last for a long time if there is a fission of the polar vortex.

After this fission, these blocks settle in regions and habitats after approximately several weeks have passed and shape the weather patterns for the remainder and until the end of the winter season, so that certain areas are exposed to storms and rainy depressions, and others are stable and warm. It is worth noting that the period during which the sudden warming occurs and the aforementioned aftershocks are proportional, this period becomes low-resolution global weather models due to the randomness of the distribution of polar air until it stabilizes in specific locations, with which the computer weather forecast models return to their usual accuracy, and the conversation here is more. Especially about the computer weather forecast models for the medium and long terms. The effects of this phenomenon vary from year to year according to other weather elements and indicators prevailing in the world at the time of this phenomenon, from the prevalence of the phenomenon of laninia, which is represented by the decrease in surface temperatures of the waters of the equatorial part of the Pacific Ocean, the locations and intensity of the Madden-Julian waves (MJO), And many other elements enter either the temperatures of the water bodies in the northern hemisphere or the regions of depressions and the prevailing patterns at the time. Weather experts always try to predict how a sudden stratospheric warming will affect weather patterns after their occurrence, based on the above, but in many cases the effect is not what was expected, but it strikes some times.

Although it is climatic and statistically speaking, this phenomenon usually means the accumulation of polar coldness in the western European continent and sometimes eastern Canada all the way to the east of the United States of America, but this time it seems that the accumulation of polar cold will occur in the east of the European continent in the end. Atmospheric simulation computer modeling senses. All of the above and due to its direct impact on the weather patterns in the northern hemisphere, the Arab world is directly affected by the consequences of this phenomenon, as it is expected as a result that the distribution of air masses will be in the first days following the occurrence of this phenomenon (i.e. the first two weeks of January (January 2021) that the northwestern African regions (the Maghreb) will be affected by successive cold, rainy and snowy polar depressions, in addition to the western European continent, which is expected to witness many of its capitals such as Paris and London and even Madrid in the south. High snowfall, corresponding to the flow of very warm currents to the western parts of the Arab East, including the Levant, including Jordan and Egypt, in addition to Libya, and this is behind the expectations of the Arab Weather Center that dry, stable and perhaps warm weather will prevail in some The times are unusual in these countries in the first part of January of the year 2021, and at the same time, and as a consequence of the same situation, cold currents flow from the north of the Asian continent to the Arabian Gulf and central and southern Arabia. Causing a significant drop in temperatures below the usual levels in those areas, which may reach close to zero degrees Celsius in the high mountains of the Sultanate of Oman.

After that, and after the consequences of this fission of the polar vortex have stabilized, it is believed that the polar air with multiple sources will accumulate for a not simple period in the eastern European regions, but some computer modeling went to predict the centering of one of the polar vortex centers there, which will have a direct impact at the time on the Arab East. Where the air systems are expected to change and their reflection, perhaps literally, so that the regions of the Levant, the eastern Mediterranean, and the central, northern and western parts of the Arabian Peninsula will be exposed to rainy depressions and perhaps some of them are cool enough to cause snowfalls in some areas, while It is expected that the temperatures will rise and the weather is relatively stable in the Maghreb, and the temperatures will be relatively higher in southeastern Arabia. But due to the presence of other factors involved in controlling the formulation of weather patterns, it is also expected that the shape of the prevailing atmospheric pattern in the last period of the month will be complex, represented by a large accumulation of polar cold in the east of the European continent with a strong polar vortex there, but the atmospheric pattern may lack To the presence of strong heights sufficient to push part of these cold blocs in the eastern European continent to the Arab East, which leads us to expect the prevalence of a natural winter atmosphere in the fourth week of the month.

And at all times and as a summary, it has become certain that there will be an unusual warmth in large parts of the Arab East in the first part of the month and a corresponding return to the normal winter in the second part of the month, while it is believed that the matter will be the opposite in the Maghreb, where the polar cold The depressions in the first part of the month and offset by a more stable and warmer atmosphere in the second part of the month.

In view of some other factors in the atmosphere of those interested that contribute to the crystallization of the atmosphere, computer modeling projections indicate that the coefficients of fluctuations in January of 2021 will be as follows:

1. North Atlantic Coefficient (NAO): The negative phase most days of the month, but indications are that it will approach the neutral phase at the end of the month.
   
   • The effect of the main parameter statistically at this stage alone (without taking the rest of the coefficients) with a correlation coefficient of more than 90% is: temperatures cooler than usual in the eastern and central European continent, and warmer than usual in the Arab East.
2. Arctic Oscillation Coefficient (AO): The negative phase most days of the month, but indications are moving that it will approach the neutral phase at the end of the month.
   
   • The effect of the main parameter statistically at this stage alone (without taking the rest of the coefficients) with a correlation coefficient of more than 90% is: temperatures cooler than usual in the eastern and central European continent, and warmer than usual in the Arab East.
3. Northern Atlantic water surface temperature coefficient (AMO): significantly positive .
   
   • The statistically significant effect of the main parameter at this stage alone (without taking the rest of the coefficients), with a correlation coefficient of more than 90%, is: temperatures warmer than usual in the Levant.
4. The laninia phenomenon: the negative phase of the weak and a decrease in the strength of the laninia phenomenon towards the weak phase.
   
   • The effect of the main parameter statistically at this stage alone (without taking the rest of the coefficients) with a correlation factor of more than 90% is: There is no effect within the specified correlation factor.
5. Pacific Northern Water Surface Temperature Oscillation Coefficient (PDO): negative phase.
   
   • The effect of the main parameter statistically at this stage alone (without taking the rest of the coefficients) with a correlation coefficient of more than 90% is: Temperatures cooler than usual in the Levant.
6. Indian Ocean Oscillation Index (IOD): neutral phase.
   
   • The main laboratory effect statistically at this stage alone (without taking the rest of the transactions) correlation coefficient of more than 90% is: no.
7. Zones wind oscillation factor (QBO): positive / westerly phase.
   
   • The main laboratory effect statistically at this stage alone (without taking the rest of the transactions) correlation coefficient of more than 90% is: a little than usual on the Levant degrees colder temperatures.

God knows