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مباحث عمومی هواشناسی
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- تاریخ شروع
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شبیه بادسنج دستیه
Amir Mohsen
متخصص بخش هواشناسی
[h=2]London England Winter Forecast 2013-2014 by Meteorologist Rob Guarino September 1, 2013
OUR AWARDS...20 YEARS OF FORECASTING
This is an early look at the Winter Outlook 2013-2014. We are looking at the Big 3 Factors that will carve out this winter. We have been doing this for over 20 years.
1. EL NINO (NOW IS NEUTRAL)
2. ARCTIC (ARCTIC OSCILLATION)
3. NAO (NORTH ATLANTIC OSCILLATION)
The NAO is a very important factor to get right in order to have a shot at verifying on the winter forecast for London. Going back to the colder years with snow we can see how the NAO reacted:
Cold Winters
DJF= -1.32, -2.12, -0.96
DJF= -1.93, -1.11, -1.98
Warm Winters
DJF= 0.61, 1.17, 2.00
DJF= 1.34, 0.22, -0.47
OTHER FACTORS INVOLVING NAO
نه :خجالت2:
اواسط سپتامبر
به دنبال ناهنجاری های بارش پاییزه نقاط مختلف کشور که عملاْ باعث ریزش های بیش از حد معمول در اکثر نواحی کشور گردید و آنومالی های دمایی و بارش برف زمستانه را به دنبال دارد همانگونه که در مقالات و آثار قبلی به آن اشاره گردیده همگی نشان از بروز رویداد ال نینو دارد که از ماه اکتبر در حال تکوین بوده است. این رویداد با رویداد سال۸۷-۱۹۸۶برابر است و می تواند یک رویداد متوسط تلقی گردد.
چه عاملى باعث ميشود تا برخى از پاييزها همانند پاييز ١٣٨٥ ( النينو ) و پاييز ١٣٩٠ ( لانينا ) زمستانى شوند ؟
آبان و آذر ١٣٨٥ و آبان ١٣٩٠ چه اتفاقى در جو رخ داد كه اين ماه ها زمستانى شدند ؟
پاسخ : ببینید علل تشکیل سیستم پرفشار و به‌واسطه آن آغاز بارش‌های سنگین برف و باران، به بررسی‌های کارشناسانه بیشتری احتیاج دارد. با وجود این نمی‌توان از کنار تغییر زودهنگام کمربند همگرایی فشار گذشت. در واقع می‌توان گفت که چنانچه این کمربند کمی زودتر از موعد مقرر جابه‌جا شود و بين ریزش هوای سرد قطب روی مدیترانه و توده گرمایی آمده از سمت استوا در مدیترانه برهمکنش صورت بگيرد اين الگو باعث زمستانى شدن پاييز ميشود .
در واقع شكل گيرى بندال امگا باعث وقوع ناهنجارى زمستانه در پاييز ميشود پس زمستانى شدن برخى از پاييزها ربط زيادى به شرايط انسو نداره.
چه عاملى باعث ميشود تا برخى از پاييزها همانند پاييز ١٣٨٥ ( النينو ) و پاييز ١٣٩٠ ( لانينا ) زمستانى شوند ؟
آبان و آذر ١٣٨٥ و آبان ١٣٩٠ چه اتفاقى در جو رخ داد كه اين ماه ها زمستانى شدند ؟
پاسخ : ببینید علل تشکیل سیستم پرفشار و به‌واسطه آن آغاز بارش‌های سنگین برف و باران، به بررسی‌های کارشناسانه بیشتری احتیاج دارد. با وجود این نمی‌توان از کنار تغییر زودهنگام کمربند همگرایی فشار گذشت. در واقع می‌توان گفت که چنانچه این کمربند کمی زودتر از موعد مقرر جابه‌جا شود و بين ریزش هوای سرد قطب روی مدیترانه و توده گرمایی آمده از سمت استوا در مدیترانه برهمکنش صورت بگيرد اين الگو باعث زمستانى شدن پاييز ميشود .
در واقع شكل گيرى بندال امگا باعث وقوع ناهنجارى زمستانه در پاييز ميشود پس زمستانى شدن برخى از پاييزها ربط زيادى به شرايط انسو نداره.
Amir Mohsen
متخصص بخش هواشناسی
Arctic Temperatures
Daily Mean Temperatures North of 80 degree North.
Daily Mean Temperatures North of 80 degree North.
على جان منظورم بارشى كه از شمال غرب تا جنوب شرق را پوشش بده و چشمگير باشه
علیرضا موقری; دانشجوی دکترای آب و هواشناسی در برنامه ریزی محیطی فعالیت در زمینه های سینوپتیک، دینامیک، سنجش ماهواره ای
http://climatologist.blogfa.com/
http://www.ardebilmet.ir/to/in/ahtml/44-5-software.htm
http://www.liveweatherblogs.com/
http://climatologist.blogfa.com/
http://www.ardebilmet.ir/to/in/ahtml/44-5-software.htm
http://www.liveweatherblogs.com/
Amir Mohsen
متخصص بخش هواشناسی
Image of the Day
Amir Mohsen
متخصص بخش هواشناسی
Cooler Pacific Ocean May Explain Climate Change Paradox
By Denise Chow, Staff Writer | August 28, 2013 02:42pm ET
Cooling sea-surface temperatures in the tropical Pacific Ocean — a phase that is part of a natural warm and cold cycle — may explain why global average temperatures have stabilized in recent years, even as greenhouse gas emissions have been warming the planet, according to new research.
The findings suggest that the flattening in the rise of global temperatures recorded over the past 15 years are not signs of a "hiatus" in global warming, but are tied to cooling temperatures in the tropical or equatorial Pacific Ocean. When the tropical Pacific naturally switches back into a warm phase, the long-term trends in global warming, including more steeply rising global temperatures, will likely increase, said study co-author Shang-Ping Xie, a climate scientist at the University of California, San Diego.
"The engine driving atmospheric circulation on global scales resides in the tropical Pacific," Xie told LiveScience. "When the natural cycle shifts the next time to a warmer state, we're going to see more extreme warming on the global scale." [The Reality of Climate Change: 10 Myths Busted]
A climate paradox
In early May, a carbon dioxide monitor in Hawaii recorded the proportion of carbon dioxide in the atmosphere as being more than 400 parts per million (ppm) for the first time in human history, breaking a 3-million-year-old record. (Parts per million means that, in this example, for every million molecules of air, 400 of them are carbon dioxide.) But, over the past 15 years, global average temperatures have stabilized rather than sharply increased, as previous predictions suggested they should have, mystifying climate scientists and adding fuel to the fire for climate change skeptics.
"We had this puzzle — the concentration of carbon dioxide was over 400 ppm, last year we had record summer heat waves in the U.S., record retreat of Arctic sea ice. All of these things are consistent with the general warming of the climate," Xie said. "Yet, if you plot the global temperature, you see a flattening average over the last 15 years. On the one hand, scientists are saying carbon dioxide is causing the general rise of global temperatures, but on the other hand, in recent years there is no warming, so something very strange is going on."
Xie and his colleagues set out to solve this mystery using climate models to reproduce the long- and short-term trends based on global climate records from the past 130 years. The researchers found that sea-surface temperatures in the tropical Pacific Ocean, in spite of anthropogenic or manmade effects of global warming, were key ingredients in creating the flattening global temperatures seen in the past 15 years.
"In our model, we were able to show two forces: anthropogenic forces to raise global average temperature, and equatorial Pacific cooling, which tries to pull the temperature curve down, almost like in equilibrium," Xie said.
The effect is similar to the El Niño and La Niña cycles, which are parts of a natural oscillation in the ocean-atmosphere system that occur every three to four years, and can impact global weather and climate conditions, Xie explained. El Niño is characterized by warmer-than-average temperatures in the waters of the equatorial Pacific Ocean, while La Niña typically features colder-than-average waters.
The warm and cool phases in the Pacific Ocean studied by Xie and his colleagues appear to last much longer than the El Niño and La Niña cycles. Previously, the Earth experienced cooling in the tropical Pacific from the 1940s to the 1970s, before oscillating into a warm state from the 1970s to the 1990s.
Current scientific models are unable to predict when the current cooling period will end, Xie said, but when the ocean swings back into a warm phase, parts of the planet may experience warmer temperatures.
"The equatorial Pacific Ocean is associated with distinct regional patterns, like the Pacific coast of North America," Xie said. "Because of equatorial cooling, this area has not been warming as rapidly as before, but when the equatorial Pacific shifts into a warm state, those regions might expect rapid warming, on the order of 2 degrees Celsius [3.6 degrees Fahrenheit] over 15 years."
Implications for a warming planet
Scientists have known that the eastern equatorial Pacific Ocean takes in a significant amount of heat from the atmosphere, but this new study suggests this small portion of the world's oceans could have a big influence on global climate, said James Moum, a professor of physical oceanography at Oregon State University in Corvallis, Ore., who was not involved with the new study.
While the models used in the study rely on some assumptions (for instance, the researchers set the sea-surface temperature to what is observed, rather than computing the temperatures, as would be done in a numerical model), Moum called the research "a brave experiment."
"It provides a physical basis for the current global mean temperature leveling off, while at the same time, points to this equatorial cold tongue as being the major driver for that," Moum told LiveScience.
There are still many unknowns about how this warming and cooling in the Pacific Ocean interacts with man-made greenhouse gas emissions to change the Earth's climate.
"We had El Niñolong before we had anthropogenic forcing — they occur independently of man-made forcing, certainly," Moum said. "Whether they're amplified by it is another question. The flip side of the story is that if this part of the ocean has an outside influence when it cools, it's going to have an outside influence when it warms. It's definitely suggested in the paper that this is a cause for concern."
The detailed findings of the study were published online today (Aug. 28) in the journal Nature.
By Denise Chow, Staff Writer | August 28, 2013 02:42pm ET
|
A thermometer in the Earth shows increasing global climate sensitivity.Credit: Eduard Härkönen | Shutterstock View full size image |
The findings suggest that the flattening in the rise of global temperatures recorded over the past 15 years are not signs of a "hiatus" in global warming, but are tied to cooling temperatures in the tropical or equatorial Pacific Ocean. When the tropical Pacific naturally switches back into a warm phase, the long-term trends in global warming, including more steeply rising global temperatures, will likely increase, said study co-author Shang-Ping Xie, a climate scientist at the University of California, San Diego.
"The engine driving atmospheric circulation on global scales resides in the tropical Pacific," Xie told LiveScience. "When the natural cycle shifts the next time to a warmer state, we're going to see more extreme warming on the global scale." [The Reality of Climate Change: 10 Myths Busted]
A climate paradox
In early May, a carbon dioxide monitor in Hawaii recorded the proportion of carbon dioxide in the atmosphere as being more than 400 parts per million (ppm) for the first time in human history, breaking a 3-million-year-old record. (Parts per million means that, in this example, for every million molecules of air, 400 of them are carbon dioxide.) But, over the past 15 years, global average temperatures have stabilized rather than sharply increased, as previous predictions suggested they should have, mystifying climate scientists and adding fuel to the fire for climate change skeptics.
"We had this puzzle — the concentration of carbon dioxide was over 400 ppm, last year we had record summer heat waves in the U.S., record retreat of Arctic sea ice. All of these things are consistent with the general warming of the climate," Xie said. "Yet, if you plot the global temperature, you see a flattening average over the last 15 years. On the one hand, scientists are saying carbon dioxide is causing the general rise of global temperatures, but on the other hand, in recent years there is no warming, so something very strange is going on."
Xie and his colleagues set out to solve this mystery using climate models to reproduce the long- and short-term trends based on global climate records from the past 130 years. The researchers found that sea-surface temperatures in the tropical Pacific Ocean, in spite of anthropogenic or manmade effects of global warming, were key ingredients in creating the flattening global temperatures seen in the past 15 years.
"In our model, we were able to show two forces: anthropogenic forces to raise global average temperature, and equatorial Pacific cooling, which tries to pull the temperature curve down, almost like in equilibrium," Xie said.
The effect is similar to the El Niño and La Niña cycles, which are parts of a natural oscillation in the ocean-atmosphere system that occur every three to four years, and can impact global weather and climate conditions, Xie explained. El Niño is characterized by warmer-than-average temperatures in the waters of the equatorial Pacific Ocean, while La Niña typically features colder-than-average waters.
The warm and cool phases in the Pacific Ocean studied by Xie and his colleagues appear to last much longer than the El Niño and La Niña cycles. Previously, the Earth experienced cooling in the tropical Pacific from the 1940s to the 1970s, before oscillating into a warm state from the 1970s to the 1990s.
Current scientific models are unable to predict when the current cooling period will end, Xie said, but when the ocean swings back into a warm phase, parts of the planet may experience warmer temperatures.
"The equatorial Pacific Ocean is associated with distinct regional patterns, like the Pacific coast of North America," Xie said. "Because of equatorial cooling, this area has not been warming as rapidly as before, but when the equatorial Pacific shifts into a warm state, those regions might expect rapid warming, on the order of 2 degrees Celsius [3.6 degrees Fahrenheit] over 15 years."
Implications for a warming planet
Scientists have known that the eastern equatorial Pacific Ocean takes in a significant amount of heat from the atmosphere, but this new study suggests this small portion of the world's oceans could have a big influence on global climate, said James Moum, a professor of physical oceanography at Oregon State University in Corvallis, Ore., who was not involved with the new study.
While the models used in the study rely on some assumptions (for instance, the researchers set the sea-surface temperature to what is observed, rather than computing the temperatures, as would be done in a numerical model), Moum called the research "a brave experiment."
"It provides a physical basis for the current global mean temperature leveling off, while at the same time, points to this equatorial cold tongue as being the major driver for that," Moum told LiveScience.
There are still many unknowns about how this warming and cooling in the Pacific Ocean interacts with man-made greenhouse gas emissions to change the Earth's climate.
"We had El Niñolong before we had anthropogenic forcing — they occur independently of man-made forcing, certainly," Moum said. "Whether they're amplified by it is another question. The flip side of the story is that if this part of the ocean has an outside influence when it cools, it's going to have an outside influence when it warms. It's definitely suggested in the paper that this is a cause for concern."
The detailed findings of the study were published online today (Aug. 28) in the journal Nature.
2- کوچ زودهنگام پرندگان مهاجر : سازمان محيط زيست مازندران مهر ماه ، از کوچ زودهنگام پرندگان مهاجر ساکن سيبري و مناطق سردسير شمال اروپا و روسيه خبر داد. اين نکته بسيار مهمي است و نشان مي دهد سرماي زودرس در اين مناطق و به تبع آن انتقال اين هواي سرد به سمت ايران در ماههاي بعدي است. از ياد نبريم که پرندگان ساکن مناطق سرد به دليل نقش حياتي وضع هوا در زندگيشان ، هواشناسان قابلي هستند. ( خبر براى سال ٨٦ است )
نتيجه : كوچ زودهنگام پرندگان مهاجر = زمستان بسيار سرد
پرسش : وضعيت كوچ پرندگان مهاجر الان چگونه اس؟
نتيجه : كوچ زودهنگام پرندگان مهاجر = زمستان بسيار سرد
پرسش : وضعيت كوچ پرندگان مهاجر الان چگونه اس؟
. به كرات مشاهده شده كه هرچه پوست پیاز، زیادتر و كلفت تر باشد، زمستان طولانی تر و سخت تر خواهد
بود. این امر نشان دهنده این است كه طبیعت برای حفظ گیاه پیاز از سرمای سخت زمستان، از پوشش های
ضخیم برای پوشاندن پیاز استفاده می نماید.
. چنانچه در فصل پاییز کفشدوزک های نارنجی زیاد دیده شوند زمستان خنک و اگر دیده نشوند زمستان سخت
بود. این امر نشان دهنده این است كه طبیعت برای حفظ گیاه پیاز از سرمای سخت زمستان، از پوشش های
ضخیم برای پوشاندن پیاز استفاده می نماید.
. چنانچه در فصل پاییز کفشدوزک های نارنجی زیاد دیده شوند زمستان خنک و اگر دیده نشوند زمستان سخت
در فرهنگ عامه مردم لرستان ، همچون دیگر مناطق کشورمان بنا به تجربه و نقل قول های منتقل شده ، باورهایی در بین مردم (بویژه عشایر کشاورز و دام دار) بر اساس ظواهر و نشانه های تغییرات جوی وجود داشته و دارد که برخی از آنها عبارتند از :
چنانچه در روزهای پاییز و زمستان هوا بیش از اندازه گرم و آقتاب در روز شدید و سوزان باشد ، معتقدند روز بعد باید انتظار بارندگی را داشت .اگر در بارندگی زمستان روز شنبه هوا صاف نشد و یا روز شنبه بارندگی شروع شد مردم معتقدند بارندگی در روزهای بعد از آن هم ادامه خواهد یافت.
شمه که نکردش خش
(شنبه که هوا صاف و خوش شد)
بردش سی جو رش
( هوا صاف نمی شه تا جوها سفید بشوند)
در روزهای ابری زمستان و پاییز چنانچه آسمان طرف جنوب و قبله باز و ابرها کنار رفته باشند انتظار باران در ساعات آینده نمی رود. اگر آسمان جنوب قبله را ابرهای سیاه و تیره پوشانده باشد بارندگی ادامه خواهد داشت .
چنانچه در زمستان و بهار ابرها بسوی مغرب در حرکت باشند بارندگی شدید و طولانی در پیش است . اگر ابرها از مغرب بسوی مشرق و شمال شرقی در حرکت باشند ،روزهای بعد هوا صاف و بدون بارندگی خواهد بود.
اور سور ایواره
(ابر سرخ غروب)
هف شو هف رو نواره
(۷ شب و ۷ روز نخواهد بارید)
اگر در فصل های پاییز ، زمستان و بهار در هنگام غروب آفتاب ابرهای سمت مغرب آسمان به رنگ قرمز یا نارنجی باشند ، نشانه این است که حداقل تا یک هفته بعد از آن باران نخواهد بارید و هوای صافی پیش روی است
هرگاه هاله دور ماه در شبهای مهتاب شعاع بیشتری داشته باشد یعنی دایره بزرگ بنظر برسد ، روز بعد از آن بارش باران حتمی است و چنانچه برعکس این باشد (هاله دور ماه دایره کوچک و به ماه نزدیک باشد) روز بعد از آن هوا صاف خواهد بود.
آغل دیر بارو نزیک
(دایره و آغل دور ، باران نزدیک)
آغل نزیک بارو دیر
(آغل نزدیک ، بارون دور)
Amir Mohsen
متخصص بخش هواشناسی
امیر کوروش بلا !!!!
نکنه به نقشه های من دسترسی داری؟!!!!!!!
ولی پرنده ها چقدر زود بفکر افتادان چون تازه از فوریه هوا قراره خیلی سرد بشه:
نکنه به نقشه های من دسترسی داری؟!!!!!!!
ولی پرنده ها چقدر زود بفکر افتادان چون تازه از فوریه هوا قراره خیلی سرد بشه:
- وضعیت