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مباحث عمومی هواشناسی تابستان 1393

وضعیت
موضوع بسته شده است.

Amir Mohsen

متخصص بخش هواشناسی












pc-140829-locusts-01_7bbbc9adf3d3fdb0d50c9ceb854f70dd.nbcnews-ux-1280-900.jpg

RIJASOLO / AFP - Getty Images
3 hours






Locust Cloud Darkens Skies Over Madagascar Capital
A swarm of locusts invaded the center of Madagascar's capital city on Thursday, as clouds of insects darkened the skyline of Antananarivo.
A locust plague that began over two years ago threatens the food security and livelihoods of 13 million residents of the Indian Ocean island, according to the Food and Agriculture Organization of the United Nations.




pc-140829-locusts-02_7bbbc9adf3d3fdb0d50c9ceb854f70dd.nbcnews-ux-640-360.jpg
RIJASOLO / AFP - Getty Images
A swarm of locusts flies over the center of Antananarivo, Madagascar, on August 28, 2014.
 

Amir Mohsen

متخصص بخش هواشناسی












pc-140829-volcano-papua-01_4e4c4fd7b870ded44023147ae696e88b.nbcnews-ux-1280-900.jpg

OLIVER BLUETT / AFP - Getty Images
6 hours






Volcano Erupts in Papua New Guinea, Diverts Flights
A volcanic eruption in Papua New Guinea on Friday sent smoke and ash spewing high over the South Pacific island nation, leading some aircraft to alter their flight paths.
Mount Tavurvur on East New Britain Island erupted hours before dawn, a bulletin from the Rabaul Volcanological Observatory said. There have been no reports of injuries.




pc-140829-volcano-papua-02_4e4c4fd7b870ded44023147ae696e88b.nbcnews-ux-640-600.jpg
JOYCE LESSIMANUAJA / AFP - Getty Images
Mount Tavurvur erupting in eastern Papua New Guinea on August 29, 2014. The volcano, which destroyed the town of Rabaul when it erupted simultaneously with nearby Mount Vulcan in 1994, rumbled to life early in the morning on the tip of the remote island of New Britain.​
 

Amir Mohsen

متخصص بخش هواشناسی
SoCal Surfers Stoked Over Hurricane Marie's Huge Waves


Hurricane Marie brought much higher than normal surf, sending surfers and body-boarders to catch the waves in Southern California.






  • 140827-surfing-hurricane-marie-02.nbcnews-ux-1280-800.jpg

    Chris Carlson / AP

    1 A large crowd gathers to watch surfers and body surfers ride waves at "The Wedge" on Aug. 27, 2014 in Newport Beach, Calif. Beachgoers experienced much higher than normal surf, brought on by Hurricane Marie spinning off the coast of Mexico.
  • 140827-surfing-hurricane-marie-01.nbcnews-ux-1280-900.jpg

    Chris Carlson / AP

    2 A boogieboarder rides a wave at "The Wedge" in Newport Beach.
  • 140827-surfing-hurricane-marie-04.nbcnews-ux-1280-900.jpg

    Jae C. Hong / AP

    3 A man walks through flooded beachfront properties on Aug. 27, 2014, in Seal Beach, Calif. A low-lying street in the Southern California coastal community of Seal Beach has been inundated by a surge of rising seawater brought on by Hurricane Marie.



    140828-california-lifeguard-station-jms-2153_093349cf9c695966232e219eb1a41d8b.nbcnews-ux-1280-800.jpg



140827-surfing-hurricane-marie-03.nbcnews-ux-1280-800.jpg
 

Amir Mohsen

متخصص بخش هواشناسی
خیلی جالبه که چقدر MJO روی اقلیم منطقه ما تاثیر گذاره!!!!!!!!!

NCPE_phase_21m_small.gif


نمودار بالا نشون میده که ما در فاز 3 وارد شدیم و آنومالی ارتفاع ژئوپتانسیل تراز 200 میلی بار در فاز 3 برای ماههای سپتامبر- اکتبر و نوامبر میشه plot زیر که با نقشه های پیش بینی اینروزها شباهت های بسیار زیادی داره:

i07q3kiq43mwh0l087l9.jpg
 

Amir Mohsen

متخصص بخش هواشناسی
خیلی جالبه که چقدر MJO روی اقلیم منطقه ما تاثیر گذاره!!!!!!!!!

NCPE_phase_21m_small.gif


نمودار بالا نشون میده که ما در فاز 3 وارد شدیم و آنومالی ارتفاع ژئوپتانسیل تراز 200 میلی بار در فاز 3 برای ماههای سپتامبر- اکتبر و نوامبر میشه plot زیر که با نقشه های پیش بینی اینروزها شباهت های بسیار زیادی داره:

i07q3kiq43mwh0l087l9.jpg




درود و عرض ادب خدمت دوستان عزیز:

kjf4ebl9dqa0k7bkgxjf.png
 

Amir Mohsen

متخصص بخش هواشناسی
ایران هم به همین شکل بود تا حدودی!!!


[h=2]2014 temperature extremes: U.S. runs hot and cold


August 29, 2014



So far in 2014, much of the United States has been unusually cold. Not only that, but much of the United States has been unusually warm.
But wait, you say, you can’t have it both ways! Can you?
Typically, the answer to that question is no. But 2014 has not been typical. Never before have such large areas of the country experienced such radically different temperature extremes as they have so far this year. The map below shows just how divergent the temperature patterns have been across the contiguous United States for January-July 2014.
jan-jul2014_mintemp_rank_610.jpg
Minimum temperature ranks for January-July 2014 within the historical record (1895-2014), from record coldest (darkest blue) to record warmest (darkest red). Map adapted from analysis by National Climatic Data Center.




Minimum temperatures (“overnight lows”) for much of the Upper Midwest and the Mississippi Valley were much cooler than average—with a lone “record coldest” minimum temperature in Oklahoma—while a number of climate divisions across the Southwest, including drought-stricken California had record warm overnight lows.
The graph below shows January-July temperature extremes in a different way: the bars represent the percent of the country experiencing extremely warm or cold average maximum temperature (“daytime high”) during the first part of each year since 1910. For this analysis, an extreme means in the top or bottom 10% of the historical range of values recorded for a location.
US_extremes_index_jan-jul2014_610.gif
Graph of percent U.S. area affected by extremes in maximum temperature (red is warm, blue is cool) in January-July 2014, based on data from the U.S. Climate Extremes Index (Step 1) from the National Climatic Data Center.




In most years in the record, extremes are significantly lopsided: a given year’s bar is mostly red or mostly blue, sometimes capped with a small segment of the opposite color. In other words, either some part of the country is experiencing warm extremes or cold extremes, but not both. Only a handful of years have a pattern similar to 2014—in which more than 10 percent of the country was experiencing extreme warmth while a similarly large or larger area experienced extreme coolness. Can you spot them all?
Even among these years, 2014 is unprecedented: never before has the country experienced such large areas of simultaneous, opposing temperature extremes in the same January-July period. At a combined 40% of the country, the area affected by extremes so far this year is nearly double the size you’d expect due to chance.
(As an aside, also notice how the graph becomes skewed toward warm extremes in more recent decades: this is yet another metric for how climate is changing.)
In an upcoming post, we will explore some of the weather and climate patterns behind the usually extreme U.S. temperatures.




 

Amir Mohsen

متخصص بخش هواشناسی
Impact of the MJO on the boreal winter extratropical circulation

Chaim I. Garfinkel1,
James J. Benedict2 and
Eric D. Maloney3

Article first published online: 28 AUG 2014

DOI: 10.1002/2014GL061094

Abstract

The effect of the Madden-Julian Oscillation (MJO) on the Northern Hemisphere wintertime stratospheric polar vortex is evaluated using a meteorological reanalysis data set and a modern atmospheric general circulation model. The MJO influences the tropospheric North Pacific; and in particular, it modulates the heat flux that is in phase with the climatological planetary waves in both the troposphere and stratosphere. The phase of the MJO in which convection is propagating into the tropical central Pacific leads to a weakened vortex, while suppressed MJO convection in this region is associated with a stronger vortex. Subsequently, the MJO modulates the phase of the tropospheric North Atlantic Oscillation (also known as the Arctic Oscillation or the Northern Annular Mode). While the responses in the model and in the reanalysis data differ in some respects, they both indicate that the MJO can remotely impact the extratropical tropospheric circulation via the stratosphere.

Impact of the MJO on the boreal winter extratropical circulation - Garfinkel - 2014 - Geophysical Research Letters - Wiley Online Library
 

Amir Mohsen

متخصص بخش هواشناسی
Polar Vortex Impact on Winter Weather
We are now discovering that there is a statistically significant link between Siberian snow cover, the strength of the winter polar vortex and winter temperatures across much of North America and northern Europe and Asia.
By using Siberian snow cover during the previous October as a predictor of the strength of the winter polar vortex, AER seasonal forecasts have exploited this relationship to more accurately predict winter temperatures across North America and Northern Eurasia. Other seasonal forecasts neglect the snow-polar vortex relationship and tend to focus solely on ENSO to predict large scale temperature patterns.
[h=3]How the Polar Vortex Affects Regional Temperatures The polar vortex is a fast flowing stream of air that circles the North Pole during the winter months in the upper atmosphere, known as the stratosphere. Often when the polar vortex is strong, temperatures are mild in the mid-latitudes across the Eastern US and Northern Eurasia; and when the vortex is weak, temperatures tend to be cold across the Eastern US and northern Europe and Asia.
[h=4](a) Weak or “Perturbed” Polar Vortex:
Jan-Feb 2010
[h=4](b) Strong Polar Vortex Example:
Dec-Jan 1988/89
jf2010-anim-250x250.gif
dj1988-anim-250x250.gif

(a) At the beginning of the animation, the polar vortex lies near the North Pole and it confines all the cold air around the Arctic. However as the animation advances in time, warm air emerges out of Siberia and shifts the polar vortex off the Pole. The polar vortex, which started out circular, becomes stretched out and elongated and even splits into two pieces. The contours show the initial flow occurs from west to east, and then the flow becomes more north and south as the cold air spills out from the Arctic into the mid-latitudes. (b) For the entire two months the polar vortex lies near the North Pole and it confines all the cold air around the Arctic. The polar vortex remains nearly perfectly round or circular and the contours show the flow of air remains west to east throughout the month.
[h=4]Strong Polar Vortex Strong is the more common state of the polar vortex. When the polar vortex is strong, this creates strong low pressure in the Arctic region. Because of the pressure difference between the Arctic and mid-latitudes, air flows into low pressure and this confines the cold air to high latitudes closer to the Arctic. Therefore it is often mild across the Eastern US, Europe and East Asia during winters when the polar vortex is strong.
During strong polar vortex, the air flow is fast and in a direction from west to east.
Low pressure in the Arctic region is referred to as the positive phase of the Arctic Oscillation (AO), which is also know as the North Atlantic Oscillation (NAO).
[h=4]Weak Polar Vortex When the polar vortex is weak or “perturbed”, the flow of air is weaker and meanders north and south (rather than west to east). This allows a redistribution of air masses where cold air from the Arctic spills into the mid-latitudes and warm air from the subtropics is carried into the Arctic. This mixing of air masses also favors more storms and snow in the mid-latitudes.
During a weak polar vortex, high pressure occurs in the Arctic region and is referred to as the negative phase of the Arctic Oscillation (AO). Air flows away from the high pressure Arctic. The north to south direction of the polar vortex carries cold Arctic air into the mid-latitudes of Eastern US, Europe and East Asia. Therefore it is cold across the Eastern US, Europe and East Asia during winters when the polar vortex is weak.
 

Amir Mohsen

متخصص بخش هواشناسی
Polar Vortex Impact on Winter Weather


We are now discovering that there is a statistically significant link between Siberian snow cover, the strength of the winter polar vortex and winter temperatures across much of North America and northern Europe and Asia.
By using Siberian snow cover during the previous October as a predictor of the strength of the winter polar vortex, AER seasonal forecasts have exploited this relationship to more accurately predict winter temperatures across North America and Northern Eurasia. Other seasonal forecasts neglect the snow-polar vortex relationship and tend to focus solely on ENSO to predict large scale temperature patterns.
How the Polar Vortex Affects Regional Temperatures

The polar vortex is a fast flowing stream of air that circles the North Pole during the winter months in the upper atmosphere, known as the stratosphere. Often when the polar vortex is strong, temperatures are mild in the mid-latitudes across the Eastern US and Northern Eurasia; and when the vortex is weak, temperatures tend to be cold across the Eastern US and northern Europe and Asia.
(a) Weak or “Perturbed” Polar Vortex:
Jan-Feb 2010

(b) Strong Polar Vortex Example:
Dec-Jan 1988/89

jf2010-anim-250x250.gif
dj1988-anim-250x250.gif
(a) At the beginning of the animation, the polar vortex lies near the North Pole and it confines all the cold air around the Arctic. However as the animation advances in time, warm air emerges out of Siberia and shifts the polar vortex off the Pole. The polar vortex, which started out circular, becomes stretched out and elongated and even splits into two pieces. The contours show the initial flow occurs from west to east, and then the flow becomes more north and south as the cold air spills out from the Arctic into the mid-latitudes. (b) For the entire two months the polar vortex lies near the North Pole and it confines all the cold air around the Arctic. The polar vortex remains nearly perfectly round or circular and the contours show the flow of air remains west to east throughout the month.
Strong Polar Vortex

Strong is the more common state of the polar vortex. When the polar vortex is strong, this creates strong low pressure in the Arctic region. Because of the pressure difference between the Arctic and mid-latitudes, air flows into low pressure and this confines the cold air to high latitudes closer to the Arctic. Therefore it is often mild across the Eastern US, Europe and East Asia during winters when the polar vortex is strong.
During strong polar vortex, the air flow is fast and in a direction from west to east.
Low pressure in the Arctic region is referred to as the positive phase of the Arctic Oscillation (AO), which is also know as the North Atlantic Oscillation (NAO).
Weak Polar Vortex

When the polar vortex is weak or “perturbed”, the flow of air is weaker and meanders north and south (rather than west to east). This allows a redistribution of air masses where cold air from the Arctic spills into the mid-latitudes and warm air from the subtropics is carried into the Arctic. This mixing of air masses also favors more storms and snow in the mid-latitudes.
During a weak polar vortex, high pressure occurs in the Arctic region and is referred to as the negative phase of the Arctic Oscillation (AO). Air flows away from the high pressure Arctic. The north to south direction of the polar vortex carries cold Arctic air into the mid-latitudes of Eastern US, Europe and East Asia. Therefore it is cold across the Eastern US, Europe and East Asia during winters when the polar vortex is weak.


مقایسه نقشه های آنومالی دمای سطح زمین در کنتراست با وضعیت ورتکس قطبی :

مثال 1- آنومالی دمای هوا در سطح زمین در وضعیت ورتکس قطبی قوی در طی ماههای دسامبر- ژانویه- فوریه سال 1988/89


5f3ldhj9ae3sjxq3p8g.jpg


مثال 2- آنومالی دمای سطح زمین در وضعیت ورتکس قطبی ضعیف در طی ماه ژانویه 2010

8n0stcxq1k1ln9sytoam.jpg


مثال 3- آنومالی دمای سطح زمین در وضعیت ورتکس قطبی ضعیف در طی ماه فوریه 2010

cxix9e8ksmzrf0v6px75.jpg
 

Amir Mohsen

متخصص بخش هواشناسی
Model of How Snow Cover Impacts Winter Weather
AER's winter Seasonal Forecasts rely on Siberian snow cover extent in the fall for more accurate winter predictions. Over a decade of research has allowed us to understand how variability in Siberian snow cover mostly in October can influence the weather in remote regions including the Eastern US and Europe months later. Below we show the six-step model with a timeline that begins with the advance of Siberian snow cover in October and ends with either more (less) frequent Arctic outbreaks during the winter in the Eastern US, Europe and East Asia associated with the negative (positive) phase of the large-scale telconnection pattern the Arctic Oscillation (AO).

Six_Step_Process.020-823x617.png


 

Amir Mohsen

متخصص بخش هواشناسی
Influence of the Gulf Stream on the Barents Sea ice retreat and Eurasian coldness during
early winter

Kazutoshi Sato1,2, Jun Inoue1,2,3 and Masahiro Watanabe4
1 The Graduate University for Advanced Studies, Tachikawa, Tokyo, Japan
2 Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa, Japan
3 National Institute of Polar Research, Tachikawa, Tokyo, Japan
4 Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Chiba, Japan
E-mail: sato.kazutoshi@nipr.ac.jp
Received 2 May 2014, revised 24 July 2014
Accepted for publication 25 July 2014
Published 15 August 2014
Abstract
Abnormal sea-ice retreat over the Barents Sea during early winter has been considered a leading
driver of recent midlatitude severe winters over Eurasia. However, causal relationships between
such retreat and the atmospheric circulation anomalies remains uncertain. Using a reanalysis
dataset, we found that poleward shift of a sea surface temperature front over the Gulf Stream
likely induces warm southerly advection and consequent sea-ice decline over the Barents Sea
sector, and a cold anomaly over Eurasia via planetary waves triggered over the Gulf Stream
region. The above mechanism is supported by the steady atmospheric response to the diabatic
heating anomalies over the Gulf Stream region obtained with a linear baroclinic model. The
remote atmospheric response from the Gulf Stream would be amplified over the Barents Sea
region via interacting with sea-ice anomaly, promoting the warm Arctic and cold Eurasian
pattern.

http://iopscience.iop.org/1748-9326/9/8/084009/pdf/1748-9326_9_8_084009.pdf
 

سیبری

کاربر ويژه
بالاخره در بامدادان 9 شهریور 93 بادهای شمالی این قاصدان خزان ، عطر پاییز و بوی سرزمینهای سرد شمالگان زمین رو برای یک سوم شمالی ایران به ارمغان آورد
 

golil

کاربر ويژه
با سلام
صبح با طراوتی که هر کسی سر حال ی کنه را شروع کردیم وزش باد ملایم و هوای بسیار خوبی است خداکنه بارونش هم بیاد
 

Amir Mohsen

متخصص بخش هواشناسی
درود
کلات نادر هم از صبح زود وزش باد نسبتا شدید شمال غربی در جریان هست که تا حدودی گرد و غبار هم ایجاد کرده و البته لکه های ابر که در امتداد کوههای هزار مسجد و کوپه داغ در حال شکل گیری هستند هم دیده میشه
 
وضعیت
موضوع بسته شده است.
بالا