• توجه: در صورتی که از کاربران قدیمی ایران انجمن هستید و امکان ورود به سایت را ندارید، میتوانید با آیدی altin_admin@ در تلگرام تماس حاصل نمایید.

مباحث عمومی هواشناسی

وضعیت
موضوع بسته شده است.

pokerface

متخصص هواشناسی
ممنون از لطف همیشگی شما نسبت به بنده،راستش منم در مورد این نوسانات دورپیوندی تازه در حال کسب اطلاعات اولیه هستم.اگر بشه هر مبحث با اقلیم و الگوهای جوی کشور عزیزمون تطبیق داده بشه کار جالبیه،امیر جان می‌شه برای نمونه طیّ ۴۰ ساله اخیر این نمودار میله‌ای رو برای ۵ شهر از ۵ ناحیهٔ متفاوت اقلیمی ایران رسم کنید؟
 

Amir Mohsen

متخصص بخش هواشناسی
ممنون از لطف همیشگی شما نسبت به بنده،راستش منم در مورد این نوسانات دورپیوندی تازه در حال کسب اطلاعات اولیه هستم.اگر بشه هر مبحث با اقلیم و الگوهای جوی کشور عزیزمون تطبیق داده بشه کار جالبیه،امیر جان می‌شه برای نمونه طیّ ۴۰ ساله اخیر این نمودار میله‌ای رو برای ۵ شهر از ۵ ناحیهٔ متفاوت اقلیمی ایران رسم کنید؟

خواهش میکنم بهروز جان

راستش بصورت نمودار میله ای نمی تونم ولی به شکل تاثیر بر روی نقشه ایران به صورت درصد افزایش و یا کاهش آنومالی بارش در ماههای مختلف سال واسم امکان پذیره:خجالت2:
 

هواكده

کاربر ويژه
اميرمحسن هرچه ميزان بارش برف اوراسيا در اكتبر بيشتر باشه اين يعنى زمستان پربرف براى خاورميانه

اينو ميگم شايد بهم بخندن چند روزه مورچه هاى حياط مون ناپديد شدن اين هيچى پرنده ها زود اومدن به سمت جنوب ايران
 

Amir Mohsen

متخصص بخش هواشناسی
اميرمحسن هرچه ميزان بارش برف اوراسيا در اكتبر بيشتر باشه اين يعنى زمستان پربرف براى خاورميانه

اينو ميگم شايد بهم بخندن چند روزه مورچه هاى حياط مون ناپديد شدن اين هيچى پرنده ها زود اومدن به سمت جنوب ايران

امیر کوروش عزیز

این پدیده ای رو که گفتید یعنی پوشش برف آسیای میانه در ماه اکتبر با شاخصی به اسم SAI Index یا SNOW ADVANCED INDEX می سنجند که فکر کنم یک شاخص نوظهوری هست که از 2 تا سال پیش در امریکا مورد توجه قرار گرفته .

با توجه به مقالاتی که در این زمینه خوندم هرچه میزان پوشش برف در منطقه آسیای میانه و سیبری در ماه اکتبر بیشتر باشه، میشه به وقوع زمستانهایی با سرمای سخت در عرضهای میانه جغرافیایی نیمکره شمالی امیدوار شد.
 

Amir Mohsen

متخصص بخش هواشناسی


امیر کوروش عزیز

این پدیده ای رو که گفتید یعنی پوشش برف آسیای میانه در ماه اکتبر با شاخصی به اسم SAI Index یا SNOW ADVANCED INDEX می سنجند که فکر کنم یک شاخص نوظهوری هست که از 2 تا سال پیش در امریکا مورد توجه قرار گرفته .

با توجه به مقالاتی که در این زمینه خوندم هرچه میزان پوشش برف در منطقه آسیای میانه و سیبری در ماه اکتبر بیشتر باشه، میشه به وقوع زمستانهایی با سرمای سخت در عرضهای میانه جغرافیایی نیمکره شمالی امیدوار شد.



Snow Advance Index: A New Tool for Predicting Winter’s Severity
Judah Cohen, PhD


November 14, 2011


Judah%20cropped.jpg



[h=4]Snow Advance Index: A New Tool for Predicting Winter’s Severity Researchers at AER have developed a new Snow Advance Index that could greatly improve the accuracy of winter seasonal forecasts. Based on research and testing, this index for the first time can accurately predict the severity of the upcoming winter. What makes this discovery so significant is that advances in seasonal forecasting have remained elusive, and for much of the United States seasonal forecasts are no more accurate today then they were decades ago.
[h=4]Benefit to industry and government Because weather impacts so many industries, this research and the inclusion of the Snow Advance Index in seasonal forecasts have direct benefit for businesses and government agencies that use long-range forecasts to optimize their operations and financial results and mitigate risk. Demonstrating this need, a recent report issued by the National Academy of Sciences on climate prediction concluded that more accurate climate forecasts would provide great benefit to society and would improve decision making from the agriculture to the energy sector.

Winter-Severity-Index-699x366.gif

[h=4]Why has accurate seasonal forecasting been so difficult? Significant improvements have been made in short term weather forecasting. People rely on the nightly broadcast of the seven day weather forecast, which is more often correct than not.
In contrast, making accurate seasonal forecasts continues to frustrate the large government forecast centers. Despite the use of ever more sophisticated climate models, the only demonstrable skill is that associated with the El Niño/Southern Oscillation (ENSO). Yet the temperature forecast accuracy related to ENSO is limited to western North America; and climate model forecasts for the Eastern US, Europe and East Asia remain no better than using past history or even a coin flip as a forecast tool.
[h=4]Predicting the North Atlantic Oscillation or Arctic Oscillation (N/AO) The scientific community acknowledges that a different climate phenomenon is strongly related to the weather in the Eastern US and Europe. It’s known as the North Atlantic Oscillation or Arctic Oscillation (N/AO) and is explained below.
Until now, the N/AO has been considered unpredictable; but this new Snow Advance Index developed at AER can, for the first time, predict the N/AO with a high degree of accuracy. Even more importantly, the Snow Advance Index predicts with unprecedented accuracy winter temperatures and thus the severity of winter weather in the Eastern US, Europe and East Asia. This is discussed below and shown in the Figure.
[h=4]How the N/AO impacts temperatures in Eastern US, Europe and East Asia The N/AO can be thought of as a winter severity index.

  • When the N/AO index is high, winters in the Eastern US, Europe and East Asia are milder or less severe.

  • In contrast, when the N/AO index is low, winters in the Eastern US, Europe and East Asia are more severe with increased bouts of cold weather and snowstorms.
The ability of forecasters to predict the N/AO, or winter severity index, would provide significantly improved temperature forecasts for the Eastern US, Europe and East Asia. Research at AER and other institutions has shown a statistical relationship between the Eurasian snow cover extent in October and the winter N/AO or the severity of winter weather.

  • When there is more Eurasian snow cover in October, the following winter N/AO is low and there is an increased frequency of severe weather in the mid-latitudes.

  • When there is less Eurasian snow cover in October, the following winter N/AO is high and there is a decrease in the frequency of severe weather in the mid-latitudes.
[h=4]AER Researchers demonstrate how the Snow Advance Index predicts the N/AO Until now only a moderate relationship has been demonstrated. However in a paper published in Geophysical Research Letters by myself and Justin Jones, a new Snow Advance Index is developed that is derived not from October mean snow cover extent, but rather as a function of how slowly or quickly the snow cover advances across Eurasia in October. This new Snow Advance Index is highly correlated with the N/AO or winter severity index (see Figure).

  • When snow cover advances rapidly across Eurasia in October, this is an indication that the upcoming winter will be more severe for the Eastern US, Europe and East Asia.

  • When snow cover advances slowly across Eurasia in October this is an indication that the upcoming winter will be milder for the Eastern US, Europe and East Asia.
[h=4]Using the Snow Advance Index to improve Forecast Skill Hindcasts or back testing of this new Snow Advance Index demonstrates great potential in both predicting the N/AO and improving winter temperature forecasts for much of the large population centers of the Northern Hemisphere.
This new Snow Advance Index will be used for the first time in the AER winter forecast for the winter season of 2011-2012.
[h=4]The link between the N/AO and Winter Severity The N/AO can be thought of as an index of high latitude blocking.

  • When the N/AO is high, high latitude blocking is much less frequent. The Jet Stream flows quickly from west to east carrying weather systems along quickly and acts as a divide between cold air to the north and warm air to the south. The Eastern US, Europe and East Asia, which lie in the mid-latitudes, experience long stretches of mild weather, as they remain cut off from cold, Arctic air masses.

  • When the N/AO is low, high latitude blocking is more frequent. The flow of air in the atmosphere is impeded or becomes blocked and the Jet Stream is diverted from its normal trajectory and meanders north and south around the high latitude blocking. Mixing of air masses occurs with warm air flowing north into the Arctic and cold air flowing south into the midlatitudes. The Eastern US, Europe and East Asia, which lie in the mid-latitudes experience more severe winter weather, as Arctic air masses repeatedly drive southward. Furthermore, the mixing of warm and cold air masses fuel storms and with more abundant cold air, the precipitation from these storms often falls as snow.
 

Amir Mohsen

متخصص بخش هواشناسی
Snow Advance Index (SAI)

During October we look for a number of factors which help us to determine the possible general state of the atmosphere leading in to the winter months. One of these, called the Snow Advance Index, measures the rate of advance of the permanent snow cover for the winter across Russia and Asia. The faster the rate of this advance, the more likely it is that during the winter the UK will experience some spells of cold weather, owing to various feedback mechanisms within the Earth’s atmosphere, ultimately leading to an event known as a Sudden Stratospheric Warming.
 

Amir Mohsen

متخصص بخش هواشناسی
Profile for Ludovic Brucker
Click image to view larger version.
Affiliation: GESTAR, Universities Space Research Association
Contact: E-mail
NASA Goddard Space Flight Center
Cryospheric Sciences Laboratory, Code 615
Greenbelt, MD 20771

Office Phone: 301-614-6748
Fax: 301-614-5644
[h=2]Research InterestsDr. Brucker's research focuses on the investigation of the Earth's polar climate evolution by interpreting air- and space-borne measurements of snow-covered polar and sub-polar regions (such as sea ice, ice sheets and terrestrial snowpacks) to provide climate-related variables for the satellite era. To that end, he works on developing algorithms to estimate snow properties from space using state-of-the-art multilayer snow evolution and emission models. Specifically, Dr. Brucker's current objectives are:

  • to advance, and validate, snow-depth-on-first- and multi-year-ice retrievals from the Advanced Microwave Scanning Radiometer for Earth Observing System (AMSR-E) using Operation IceBridge measurements;
  • to contribute to the comprehension of the relationships between microwave space-borne observations and snow physical properties using modeling approaches.
[h=2]BiographyDr. Brucker joined the NASA GSFC as a Research Associate in early 2010 with University of Maryland. He is now a Scientist II with Universities Space Research Association. He obtained a M.Sc. in Physics from the University of Clermont-Ferrand, France in 2006 and his Ph.D in October 2009 from the Laboratoire de Glaciologie et Geophysique de l'Environnement (LGGE), Grenoble University/CNRS, France. He conducted researches on the passive microwave emission modeling of snowpacks over Antarctica and North America. Dr. Brucker participated in two polar deployments. Currently, he focuses his activities on snow over sea ice in order to enhance snow depth retrievals using a combination of passive and active space-borne measurements, and models.
[h=2]Field Work
  • 2013 Initial Investigation of the Greenland Perennial Firn Aquifer (PFA), Southeast Greenland
  • 2011 Satellite Era Accumulation Traverse (SEAT), West Antartica
  • 2008 International Polar Year field campaign “Variability and change in the Canadian cryosphere: a contribution to state and fate of the Cryosphere”, Schefferville, Québec, Canada
  • Glaciological surveys, Chamonix, France
 

هواكده

کاربر ويژه
http://www.sid.ir/Fa/VEWSSID/J_pdf/66913891903.pdf


تحليل سينوپتيكى بارشهاى فوق سنگين


طبق اين مقاله ، چنانچه دو رودباد استوايى و قطبى بهم نزديك بشوند آنگاه شاهد تشكيل ناوه عميق و قوى بارشى در كشور خواهيم بود

يادمه بهمن ٨٣ هم اصغرى گفت علت برف سنگين و باران سيل آسا روزهاى اخير علتش ادغام اين دو رودباد
 

هواكده

کاربر ويژه
تاثير بلاكينگ بر سيكلونزائى مديترانه

چنانچه يك كمربند پرفشار بر روى اروپا قرار بگيره سيستم هاى مديترانه به عرض هاى پايينتر نفوذ ميكنن و چنانچه جنب حاره اى مزاحمت ايجاد نكنه سيستم ها به راحتى كسب رطوبت كرده ( از آبهاى جنوبى ) و ايران را تحت الشعاع خود قرار مى دهند.
 

aliwinter

Banned
یه سوال مدیر ارشد با مدیر بخش چه تفاوتی داره؟از یه شخص محترم تقا ضا میشود جواب بدهد
 
آخرین ویرایش:

هواكده

کاربر ويژه
اميرمحسن جان پس ميشه نتيجه گرفت علت گرم شدن زمستان ١٣٨٨ و بسيار سرد شدن زمستان ١٣٨٦

به وضعيت


QBO , PDO , AO

مربوط ميشه
 

الیاس 92

New member
در رابطه با زمستان 1374اینجا خیلی صحبت شده از پر بارشی .اما اون سال در نیمه جنوبی ونوار مرکزی بارش مخصوصا برف خوب بود در نوار شمالی بیشتر سوز و سرما حاکم بود .مثلا تو همین خراسان شهر های جنوبی مثل بیرجندوفردوس حتی نهبندان و طبس برف میبارید.اما شهرهای شمالی بجنوردو قوچان و مشهد هوا صاف بود. این جریان بارها اون سال تکرار شد. من فکر کنم پرفشار سیبری اجازه نفوذ بارشهارو به نوار شمالی نمیداد.
 

هواكده

کاربر ويژه
وضعيت ناهنجارى بارش كشور طى پاييز ١٣٩٠ ( در تاريخ اول سپتامبر 2011 )


http://axgig.com/images/68046384462811920648.jpg


پيش بينى وضعيت دماى كشور طى زمستان ١٣٩١ ( در تاريخ اول سپتامبر 2012 )


http://axgig.com/images/47322622092343219166.jpg




پيش بينى وضعيت دماى كشور طى زمستان ١٣٩١ ( در تاريخ اول دسامبر 2012 )


http://axgig.com/images/92799661308311890894.jpg
 
وضعیت
موضوع بسته شده است.
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