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مباحث عمومی هواشناسی
- شروع کننده موضوع Amir Mohsen
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قابلی نداشت عزیزم.:گل::احترام:
اداره تحقيقات و پيش بيني هواشناسي اردبيل، اعلام كرد كه با نفوذ جريان هواي پرفشار سرد سطح زمين دماي هوا در اين استان از ۱۵ تا ۲۰ درجه سلسيوس (سانتيگراد) در اوايل هفته پيش رو كاهش مي يابد.
به گزارش ايرنا، ساكنان اردبيل در يازدهمين روز پاييز در گرمترين ساعت با هواي ۲۹درجه سانتيگراد بالاي صفر مواجه بودند كه اين گرماي كم سابقه در اين موقع از سال و در اين شهرستان بسيار سردسير به خاطر نفوذ جريان هواي كم فشار سطح زمين از عرض هاي جنوبي به منطقه و وقوع پديده گرمباد روي داده است.
معاون اداره تحقيقات و پيش بيني هواشناسي اردبيل، گفت: انتظار مي رود كه اين شرايط جوي تا اواخر وقت فردا (جمعه) در استان اردبيل و به خصوص در نقاط مركزي اين استان تداوم داشته باشد، ولي از آن به بعد با نفوذ سامانه ناپايدار جوي با منشاء درياهاي مديترانه و سياه بر تراكم ابر و مه در آسمان منطقه افزوده شده و بارش ها آغاز شوند.
علي دولتي مهر افزود: از روز شنبه با نفوذ و استقرار توده هواي سرد اروپايي در استان اردبيل به تدريج موجي از هواي ابري و مه آلود و سرد نقاط سردسير اين استان را در بر مي گيرد.
وي اظهار كرد: با توجه به تضعيف جريان كم فشار و تقويت و نفوذ جريان هواي پرفشار سطح زمين دماي هوا در قسمت وسيعي از استان اردبيل ۱۵ درجه كاهش مي يابد و در بعضي نقاط از جمله در شهرستان اردبيل اين كاهش به ۲۰ درجه نيز خواهد رسيد.
انتظار مي رود كه بارش ها در نواحي كوهستاني و سردسير به تدريج به برف تبديل شوند و ساكنان اين نقاط اولين برف پاييز امسال را چند هفته اي زودتر از موسم معمول شاهد باشند.
اين سامانه جوي تا روز سه شنبه آينده در استان اردبيل فعال خواهد بود و بيشترين اثرات بارشي و سرماي آن در روزهاي يكشنبه و دوشنبه پديدار خواهند شد.
در شامگاه پنجشنبه با وجود آنكه بيش از دو ساعت از برچيده شدن آخرين پرتوهاي آفتاب يازدهمين روز مهر ماه از گستره دشت اردبيل سپري مي شود ولي به خاطر ادامه حاكميت جريان كم فشار جنوبي هوا همچنان گرم و به شكل كم سابقه اي در اين فصل سال و اين زمان از روز ۲۸ درجه بالاي صفر است.
به لحاظ وزش شديد باد گرم از جانب جنوب غرب كه سرعت آن گاهي از ۶۶ كيلومتر در ساعت فراتر رفت، موجي از گرد و غبار در حوالي ظهر امروز فضاي شهرستان اردبيل را فرا گرفت.
با توجه به اينكه در ماه هاي تابستان امسال اغلب وزش باد شمال شرق در منطقه حاكم بود و نيز به لحاظ انجام ساخت و سازهاي بي سابقه در سطح شهر، وزش باد مخالف موجي از گرد و غبار را به شكل گردبادهاي بسيار كوچك به هوا بلند مي كند و اين موضوع سبب نشستن لايه هاي ضخيمي از خاكريزه روي لوازم منزل شده و كدبانوان خانه دار اردبيلي را به زحمت انداخته است.
اردبيل به لحاظ موقعيت جغرافيايي و قرار گرفتن در مسير سامانه ها و جريان هاي گوناگون از شرايط اقليمي و هوايي بسيار متغير و متفاوتي در مقايسه با ساير نقاط كشور برخوردار مي باشد.
ريزش سنگين برف و رسيدن سرماي هوا به منفي چندين درجه در بعضي از سال ها در نيمه اول مهر ماه در شهرستان اردبيل سابقه دارد.
به گزارش ايرنا، ساكنان اردبيل در يازدهمين روز پاييز در گرمترين ساعت با هواي ۲۹درجه سانتيگراد بالاي صفر مواجه بودند كه اين گرماي كم سابقه در اين موقع از سال و در اين شهرستان بسيار سردسير به خاطر نفوذ جريان هواي كم فشار سطح زمين از عرض هاي جنوبي به منطقه و وقوع پديده گرمباد روي داده است.
معاون اداره تحقيقات و پيش بيني هواشناسي اردبيل، گفت: انتظار مي رود كه اين شرايط جوي تا اواخر وقت فردا (جمعه) در استان اردبيل و به خصوص در نقاط مركزي اين استان تداوم داشته باشد، ولي از آن به بعد با نفوذ سامانه ناپايدار جوي با منشاء درياهاي مديترانه و سياه بر تراكم ابر و مه در آسمان منطقه افزوده شده و بارش ها آغاز شوند.
علي دولتي مهر افزود: از روز شنبه با نفوذ و استقرار توده هواي سرد اروپايي در استان اردبيل به تدريج موجي از هواي ابري و مه آلود و سرد نقاط سردسير اين استان را در بر مي گيرد.
وي اظهار كرد: با توجه به تضعيف جريان كم فشار و تقويت و نفوذ جريان هواي پرفشار سطح زمين دماي هوا در قسمت وسيعي از استان اردبيل ۱۵ درجه كاهش مي يابد و در بعضي نقاط از جمله در شهرستان اردبيل اين كاهش به ۲۰ درجه نيز خواهد رسيد.
انتظار مي رود كه بارش ها در نواحي كوهستاني و سردسير به تدريج به برف تبديل شوند و ساكنان اين نقاط اولين برف پاييز امسال را چند هفته اي زودتر از موسم معمول شاهد باشند.
اين سامانه جوي تا روز سه شنبه آينده در استان اردبيل فعال خواهد بود و بيشترين اثرات بارشي و سرماي آن در روزهاي يكشنبه و دوشنبه پديدار خواهند شد.
در شامگاه پنجشنبه با وجود آنكه بيش از دو ساعت از برچيده شدن آخرين پرتوهاي آفتاب يازدهمين روز مهر ماه از گستره دشت اردبيل سپري مي شود ولي به خاطر ادامه حاكميت جريان كم فشار جنوبي هوا همچنان گرم و به شكل كم سابقه اي در اين فصل سال و اين زمان از روز ۲۸ درجه بالاي صفر است.
به لحاظ وزش شديد باد گرم از جانب جنوب غرب كه سرعت آن گاهي از ۶۶ كيلومتر در ساعت فراتر رفت، موجي از گرد و غبار در حوالي ظهر امروز فضاي شهرستان اردبيل را فرا گرفت.
با توجه به اينكه در ماه هاي تابستان امسال اغلب وزش باد شمال شرق در منطقه حاكم بود و نيز به لحاظ انجام ساخت و سازهاي بي سابقه در سطح شهر، وزش باد مخالف موجي از گرد و غبار را به شكل گردبادهاي بسيار كوچك به هوا بلند مي كند و اين موضوع سبب نشستن لايه هاي ضخيمي از خاكريزه روي لوازم منزل شده و كدبانوان خانه دار اردبيلي را به زحمت انداخته است.
اردبيل به لحاظ موقعيت جغرافيايي و قرار گرفتن در مسير سامانه ها و جريان هاي گوناگون از شرايط اقليمي و هوايي بسيار متغير و متفاوتي در مقايسه با ساير نقاط كشور برخوردار مي باشد.
ريزش سنگين برف و رسيدن سرماي هوا به منفي چندين درجه در بعضي از سال ها در نيمه اول مهر ماه در شهرستان اردبيل سابقه دارد.
برخی شهرهای ترکیه تو 24 ساعت گذشته بیش از 100 میل بارش داشتن
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24 hours amount precipitation. 10/03/2013 at 18:00 UTC
(55 of 55 stations)
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Amir Mohsen
متخصص بخش هواشناسی
درود دوستان عزیز
تاریخ : جمعه دوازدهم مهر 1392
نویسنده : امیر محسن
نظر بدهید
انیمیشن پیش بینی آنومالی ارتفاع ژئو پتانسیل در تراز 500 میلی بار
9 دسامبر 2013 الی 26 ژانویه 2014
9 دسامبر 2013 الی 26 ژانویه 2014
Amir Mohsen
متخصص بخش هواشناسی
با توجه به به انیمشین بالا باید دسامبر و ژانویه خوبی در پیشرو باشه، خصوصا برای جنوب غرب به سمت شمال شرق
Amir Mohsen
متخصص بخش هواشناسی
مطابق با همین نقشه ها از 21 اکتبر لغایت 11 نوامبر منطقه شمال شرق ایران تحت تاثیر پی در پی ناوه های شمال شرقی اسیای میانه قرار میگیره:گل:
Amir Mohsen
متخصص بخش هواشناسی
What the New IPCC Report Means for Europe
By Freya Roberts, The Carbon Brief
Europe has been warming faster than the global average over the past 30 years, the UN's new climate report reveals.
Since 1979, Europe has been warming faster than the global average of 0.27 degrees Celsius (°C) per decade -- but some parts have been warming faster than others.
Credit: Celso Flores, Creative Commons
Last week, the Intergovernmental Panel on Climate Change (IPCC) released part one of its scientific report in full. Among some of the most significant findings from a summary of the report are that humans are responsible for at least half of the warming experienced in recent decades. The report also predicts higher sea levels and further warming worldwide if greenhouse gas emissions continue.
The full report also looks at how climate change could pan out differently across the many regions of the world. There will be much more on this when the IPCC releases the second part of its climate report in March 2014. But the first part provides some valuable insights about how climate change affects Europe.
[h=3]Changes so far Since 1979, the land in Europe has been warming faster than the global average of 0.27 degrees Celsius (°C) per decade — but some parts have been warming faster than others.
In northern Europe - the region encompassing countries such as the UK and Sweden — temperatures have risen by 0.48°C per decade. In the central Europe region, where countries like France and Germany sit, temperatures have risen 0.44°C per decade. Temperatures in southern Europe and the Mediterranean have risen a little slower, at around 0.34°C per decade.
Image by Carbon Brief, created using data from page 46 - Chapter 14 of the IPCC's Fifth Assessment Report.
In addition to the warming trend, it's also very likely — which means scientists are 90 percent certain — that Europe has experienced a greater number of warm days and nights since 1950s, according to the report. Since the 1950s, it's also likely that the number of heat waves in Europe has risen.
The IPCC report states that it's likely mid-latitude regions like Europe have, overall, experienced more rainfall since the middle of the 20th century. A number of studies the report cites suggest extreme or heavy rainfall events have become more intense and frequent in Europe, but there is some variation across regions and seasons.
Other signs of past changes in European climate are less clear, as is the case with droughts. There’s not enough data to say whether the number of droughts has changed across Europe as a whole. However certain areas, such as the Mediterranean, have likely experienced more frequent and intense droughts since 1950.
At this point, there's no clear evidence suggesting how flooding may have changed throughout Europe, but the second part of the IPCC report will discuss in greater detail how floods vary from country to country.
Similarly, there's still discussion among scientists about whether climate change has indirectly contributed to Europe's recent cold winters. The report cites a small number of studies which have linked the decline of Arctic sea ice with the changeable winter conditions in Europe. The research suggests that warming in the Arctic could weaken the jet stream — allowing cold polar air to reach south to places like Britain. More work is needed, however, before scientists can be sure of a link.
[h=3]Future prospects Greenhouse gas emissions' disruptive effects on the climate are set to continue, warns the report. In all parts of Europe, and across all the seasons, temperatures are predicted to rise. The speed of warming by the end of the century is likely to be much faster than at present.
Climate models suggest that some parts will warm faster than others, however. The IPCC report predicts that under a scenario where greenhouse gas emissions continue to rise in the near term but stabilize by the end of the century ( RCP4.5), north Europe would warm fastest.
Temperatures there are projected to rise 2.7°C higher than the 1986-2005 average by the end of the 21st century. Central Europe is projected to warm just slightly less, with temperatures rising 2.6°C. Southern parts of Europe will warm least, say the projections, with temperatures rising 2.3°C higher than 1986-2005 levels.
Image by Carbon Brief, created using data in Table 14.1 - Chapter 14 of the IPCC's Fifth Assessment Report.
Different patterns emerge when climate models simulate rainfall patterns in the future, too. North and central parts of Europe are projected to get wetter, with an average increase in rainfall of 8 and 4 percent, respectively. Again that's compared to the 1986-2005 average. Meanwhile, Southern parts of Europe are projected to become drier, with 5 percent less rainfall on average. When rain does fall it's likely to be in heavier bursts, the report says.
Image by Carbon Brief, created using data in Table 14.1 - Chapter 14 of the IPCC's Fifth Assessment Report.
As for heat waves, it is "very likely" Europe will experience longer, more frequent or more intense warm spells (or both), the report says. Recent research also included in the report suggests that the drying out of soils may actually be amplifying the problem of heat waves.
[h=3]Climate models progress Scientists writing the new report say they have much greater confidence in their ability to model past and future changes in European climate since the IPCC's last big review of science in 2007.
It's not possible to be 100 per cent certain about exactly how much warming and rainfall the continent will experience in the near term, since the region has notoriously complicated weather. Two major circulations in the atmosphere and oceans affect the European climate from one decade to the next, making it difficult to pin down changes in the short term.
But that doesn't change the long term projections in the IPCC's report. Expect more detail when part two of the IPCC report is published next March, but for now it looks like Europe's in for hotter days and heat waves, with many northern and central countries getting wetter while southern parts get drier.
This story was originally published in The Carbon Brief and was republished with their permission.
- Published: October 3rd, 2013
By Freya Roberts, The Carbon Brief
Europe has been warming faster than the global average over the past 30 years, the UN's new climate report reveals.
Since 1979, Europe has been warming faster than the global average of 0.27 degrees Celsius (°C) per decade -- but some parts have been warming faster than others.Credit: Celso Flores, Creative Commons
Last week, the Intergovernmental Panel on Climate Change (IPCC) released part one of its scientific report in full. Among some of the most significant findings from a summary of the report are that humans are responsible for at least half of the warming experienced in recent decades. The report also predicts higher sea levels and further warming worldwide if greenhouse gas emissions continue.
The full report also looks at how climate change could pan out differently across the many regions of the world. There will be much more on this when the IPCC releases the second part of its climate report in March 2014. But the first part provides some valuable insights about how climate change affects Europe.
[h=3]Changes so far Since 1979, the land in Europe has been warming faster than the global average of 0.27 degrees Celsius (°C) per decade — but some parts have been warming faster than others.
In northern Europe - the region encompassing countries such as the UK and Sweden — temperatures have risen by 0.48°C per decade. In the central Europe region, where countries like France and Germany sit, temperatures have risen 0.44°C per decade. Temperatures in southern Europe and the Mediterranean have risen a little slower, at around 0.34°C per decade.
Image by Carbon Brief, created using data from page 46 - Chapter 14 of the IPCC's Fifth Assessment Report. In addition to the warming trend, it's also very likely — which means scientists are 90 percent certain — that Europe has experienced a greater number of warm days and nights since 1950s, according to the report. Since the 1950s, it's also likely that the number of heat waves in Europe has risen.
The IPCC report states that it's likely mid-latitude regions like Europe have, overall, experienced more rainfall since the middle of the 20th century. A number of studies the report cites suggest extreme or heavy rainfall events have become more intense and frequent in Europe, but there is some variation across regions and seasons.
Other signs of past changes in European climate are less clear, as is the case with droughts. There’s not enough data to say whether the number of droughts has changed across Europe as a whole. However certain areas, such as the Mediterranean, have likely experienced more frequent and intense droughts since 1950.
At this point, there's no clear evidence suggesting how flooding may have changed throughout Europe, but the second part of the IPCC report will discuss in greater detail how floods vary from country to country.
Similarly, there's still discussion among scientists about whether climate change has indirectly contributed to Europe's recent cold winters. The report cites a small number of studies which have linked the decline of Arctic sea ice with the changeable winter conditions in Europe. The research suggests that warming in the Arctic could weaken the jet stream — allowing cold polar air to reach south to places like Britain. More work is needed, however, before scientists can be sure of a link.
[h=3]Future prospects Greenhouse gas emissions' disruptive effects on the climate are set to continue, warns the report. In all parts of Europe, and across all the seasons, temperatures are predicted to rise. The speed of warming by the end of the century is likely to be much faster than at present.
Climate models suggest that some parts will warm faster than others, however. The IPCC report predicts that under a scenario where greenhouse gas emissions continue to rise in the near term but stabilize by the end of the century ( RCP4.5), north Europe would warm fastest.
Temperatures there are projected to rise 2.7°C higher than the 1986-2005 average by the end of the 21st century. Central Europe is projected to warm just slightly less, with temperatures rising 2.6°C. Southern parts of Europe will warm least, say the projections, with temperatures rising 2.3°C higher than 1986-2005 levels.
Image by Carbon Brief, created using data in Table 14.1 - Chapter 14 of the IPCC's Fifth Assessment Report. Different patterns emerge when climate models simulate rainfall patterns in the future, too. North and central parts of Europe are projected to get wetter, with an average increase in rainfall of 8 and 4 percent, respectively. Again that's compared to the 1986-2005 average. Meanwhile, Southern parts of Europe are projected to become drier, with 5 percent less rainfall on average. When rain does fall it's likely to be in heavier bursts, the report says.
Image by Carbon Brief, created using data in Table 14.1 - Chapter 14 of the IPCC's Fifth Assessment Report. As for heat waves, it is "very likely" Europe will experience longer, more frequent or more intense warm spells (or both), the report says. Recent research also included in the report suggests that the drying out of soils may actually be amplifying the problem of heat waves.
[h=3]Climate models progress Scientists writing the new report say they have much greater confidence in their ability to model past and future changes in European climate since the IPCC's last big review of science in 2007.
It's not possible to be 100 per cent certain about exactly how much warming and rainfall the continent will experience in the near term, since the region has notoriously complicated weather. Two major circulations in the atmosphere and oceans affect the European climate from one decade to the next, making it difficult to pin down changes in the short term.
But that doesn't change the long term projections in the IPCC's report. Expect more detail when part two of the IPCC report is published next March, but for now it looks like Europe's in for hotter days and heat waves, with many northern and central countries getting wetter while southern parts get drier.
This story was originally published in The Carbon Brief and was republished with their permission.
Amir Mohsen
متخصص بخش هواشناسی
The Most Detailed Visuals of Hurricane Sandy, Revealed
By Andrew Freedman
Follow @afreedma
Scientists have recently developed awe-inspiring visualizations of Hurricane Sandy, which devastated the Northeast and Mid-Atlantic states a year ago. The visualizations, created using state-of-the-art computer models, provide some of most detailed looks at any hurricane to date.
In this 3-D map of potential temperature, relatively cool air wraps around Sandy's core near the surface (purple and blue colors), while air parcels gain heat from moisture condensing into clouds and precipitation as they ascend through the storm’s core.
Click image to enlarge. Credit: UCAR.
Scientists based at the National Center for Atmospheric Research (NCAR) in Boulder, Colo., used an advanced hurricane computer model to create mesmerizing images and animations that almost succeed in making the destructive and deadly storm appear to be a beautiful work of art.
The hurricane went through multiple phases. After rumbling through the Caribbean and striking Cuba, it veered north-northeastward just off the East Coast. The storm was officially classified as a post-tropical cyclone as of 7 p.m. EDT on Oct.29, 2012, only an hour before it made landfall, and after hurricane force winds had already begun buffeting the New York and New Jersey coastlines.
Climate Central posted the initial round of visualizations from this team in January. But now, a team including NCAR's Mel Shapiro, the National Center for Computing Applications (NCSA), Cray Computing, and the U.S. Office of Naval Research has produced addition simulations at even higher resolution.
The visualizations show how Sandy’s life cycle was unique — going through multiple tropical and non-tropical phases as it interacted with the jet stream and surface weather features, such as a cold front draped along the East Coast.
Ultra-fine-scale simulations of Sandy’s near-surface winds (upper right) and cloud-top temperatures (lower right) closely resemble the observations derived from satellite data (at left).
Click image to enlarge. Credit: UCAR.
Robert Henson, a meteorologist and science writer with the University Corporation for Atmospheric Research in Boulder published a story about the new data, explaining the many never-before-seen atmospheric interactions that it reveals.
“As Sandy moved northeast, contrasting air masses created a pseudo-frontal system along the edge of the Gulf Stream’s warm water. The vorticity, or circulation, along this frontal zone (picture an atmospheric rolling pin oriented along the Gulf Stream) was gradually ingested by Sandy and tilted into vertical vorticity (now picture the rolling pin standing on one end),” Henson wrote. “This helped the storm’s core to intensify, tighten, and regain its Category 2 status. It’s roughly similar to the smaller-scale process by which a supercell thunderstorm can ingest, tilt, and concentrate spinning air to produce storm-scale circulations (some of which can generate tornadoes).”
This intensification came as the storm was shoved westward into the U.S. by an area of blocking high pressure in northeastern Canada and a huge dip in the polar jet stream.
- Published: October 3rd, 2013, Last Updated: October 3rd, 2013
By Andrew Freedman Follow @afreedma
Scientists have recently developed awe-inspiring visualizations of Hurricane Sandy, which devastated the Northeast and Mid-Atlantic states a year ago. The visualizations, created using state-of-the-art computer models, provide some of most detailed looks at any hurricane to date.
In this 3-D map of potential temperature, relatively cool air wraps around Sandy's core near the surface (purple and blue colors), while air parcels gain heat from moisture condensing into clouds and precipitation as they ascend through the storm’s core.Click image to enlarge. Credit: UCAR.
Scientists based at the National Center for Atmospheric Research (NCAR) in Boulder, Colo., used an advanced hurricane computer model to create mesmerizing images and animations that almost succeed in making the destructive and deadly storm appear to be a beautiful work of art.
The hurricane went through multiple phases. After rumbling through the Caribbean and striking Cuba, it veered north-northeastward just off the East Coast. The storm was officially classified as a post-tropical cyclone as of 7 p.m. EDT on Oct.29, 2012, only an hour before it made landfall, and after hurricane force winds had already begun buffeting the New York and New Jersey coastlines.
Climate Central posted the initial round of visualizations from this team in January. But now, a team including NCAR's Mel Shapiro, the National Center for Computing Applications (NCSA), Cray Computing, and the U.S. Office of Naval Research has produced addition simulations at even higher resolution.
The visualizations show how Sandy’s life cycle was unique — going through multiple tropical and non-tropical phases as it interacted with the jet stream and surface weather features, such as a cold front draped along the East Coast.
Ultra-fine-scale simulations of Sandy’s near-surface winds (upper right) and cloud-top temperatures (lower right) closely resemble the observations derived from satellite data (at left).Click image to enlarge. Credit: UCAR.
Robert Henson, a meteorologist and science writer with the University Corporation for Atmospheric Research in Boulder published a story about the new data, explaining the many never-before-seen atmospheric interactions that it reveals.
“As Sandy moved northeast, contrasting air masses created a pseudo-frontal system along the edge of the Gulf Stream’s warm water. The vorticity, or circulation, along this frontal zone (picture an atmospheric rolling pin oriented along the Gulf Stream) was gradually ingested by Sandy and tilted into vertical vorticity (now picture the rolling pin standing on one end),” Henson wrote. “This helped the storm’s core to intensify, tighten, and regain its Category 2 status. It’s roughly similar to the smaller-scale process by which a supercell thunderstorm can ingest, tilt, and concentrate spinning air to produce storm-scale circulations (some of which can generate tornadoes).”
This intensification came as the storm was shoved westward into the U.S. by an area of blocking high pressure in northeastern Canada and a huge dip in the polar jet stream.
Amir Mohsen
متخصص بخش هواشناسی
Amir Mohsen
متخصص بخش هواشناسی
Amir Mohsen
متخصص بخش هواشناسی
سلام.
گرم باد و دمای بسیار بالای هوا طی دیروز باعث آتش سوزی در ارتفاعات گرگان شد. اما خدا رو شکر فعلا خبری از خسارت و آتش سوزی در سایر مناطق جنگلی سواحل کاسپین نرسیده.
هوای رشت خنک شده. از بعد از ظهر باید به تدریج منتظر آغاز بارش ها باشیم.
آتش سوزی در ارتفاعات گرگان + تصاویر
دیشب پیش دود ناشی از آتش‌سوزی در ارتفاعات شهر گرگان مردم این شهر را نگران کرد.
به گزارش خبرگزاری فارس از گرگان، ددیشب پیش دود و شعلههای آتش در ارتفاعات تپههای شهرک دخانیات گرگان مردم را نگران کرد.
این آتش‌سوزی به قدری شدت دارد که از فاصله بسیار دور نیز قابل رویت است و مردم با مشاهده این حادثه از خانه‌ها بیرون آمده و در حال تصویربرداری و اظهار نگرانی از این حادثه هستند.
خودروهای امداد و آتشنشانی به صورت مستمر در حال اعزام به منطقه برای مهار هرچه سریعتر آتش هستند.
تصاویر آتش‌سوزی از بام یکی از خانه‌های مشرف به حادثه
بنابر مشاهدات خبرنگار فارس در گرگان این آتش‌سوزی هر لحظه در حال افزایش است و تا به این لحظه از میزان خسارت جانی این حادثه اطلاعاتی در دسترس نیست.
این نکته نیز قابل ذکر است که عصر دیروز نیز نزدیک به 10 هکتار از جنگلهای شهرستان مراوه‌تپه در شرق استان گلستان طعمه حریق شد که این آتش در کمتر از چهار ساعت مهار شد.
اخبار تکمیلی در پیگیری خبرنگار فارس متعاقبا ارسال خواهد شد.
گرم باد و دمای بسیار بالای هوا طی دیروز باعث آتش سوزی در ارتفاعات گرگان شد. اما خدا رو شکر فعلا خبری از خسارت و آتش سوزی در سایر مناطق جنگلی سواحل کاسپین نرسیده.
هوای رشت خنک شده. از بعد از ظهر باید به تدریج منتظر آغاز بارش ها باشیم.
آتش سوزی در ارتفاعات گرگان + تصاویر
دیشب پیش دود ناشی از آتش‌سوزی در ارتفاعات شهر گرگان مردم این شهر را نگران کرد.
به گزارش خبرگزاری فارس از گرگان، ددیشب پیش دود و شعلههای آتش در ارتفاعات تپههای شهرک دخانیات گرگان مردم را نگران کرد.
این آتش‌سوزی به قدری شدت دارد که از فاصله بسیار دور نیز قابل رویت است و مردم با مشاهده این حادثه از خانه‌ها بیرون آمده و در حال تصویربرداری و اظهار نگرانی از این حادثه هستند.
خودروهای امداد و آتشنشانی به صورت مستمر در حال اعزام به منطقه برای مهار هرچه سریعتر آتش هستند.
تصاویر آتش‌سوزی از بام یکی از خانه‌های مشرف به حادثه
بنابر مشاهدات خبرنگار فارس در گرگان این آتش‌سوزی هر لحظه در حال افزایش است و تا به این لحظه از میزان خسارت جانی این حادثه اطلاعاتی در دسترس نیست.
این نکته نیز قابل ذکر است که عصر دیروز نیز نزدیک به 10 هکتار از جنگلهای شهرستان مراوه‌تپه در شرق استان گلستان طعمه حریق شد که این آتش در کمتر از چهار ساعت مهار شد.
اخبار تکمیلی در پیگیری خبرنگار فارس متعاقبا ارسال خواهد شد.
وضعیت وزش باد نشون می ده که در بیشتر مناطق سواحل غربی کاسپین باد شمالی کاملا غالب شده. در بخش های شمالی استان اردبیل هم باد شمال شرقی و کاسپینی غالب هست. اما خود اردبیل همچنان درگیر باد جنوب غربی و افزایش دما است:
تا چند ساعت دیگه جریانات شمالی کاملا در گیلان و اردبیل غالب میشن:
تا چند ساعت دیگه جریانات شمالی کاملا در گیلان و اردبیل غالب میشن:
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