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Monday, March 5, 2012
Radio Blackout affecting Sunlit side of the Earth
As seen from this image,the higher frequency signals are being largely attenuated due to the Radio Disturbance as the signals propogate through a disturbed ionosphere..
Mega Solar Flare from Sunspot 1429!!
AKSHAY DEORAS
SEVERE WEATHER FORECASTER
AFTER A BRIEF PERIOD OF QUIET SPACE WEATHER,OUR SUN IS WAKING UP DUE TO THE SUNSPOT AE 1429. The Sunspot is 4 times the size of the Earth.
The GOES X Ray flux is indicating a major Solar Flare in progress and a R3 Radio Blackout is in progress on the Sunlit side of the earth including here in India at the Higher Frequency
Solar disc is rotating and hence the sunspot 1429 will become geoeffective after some days... If it hurls another X class flare then that may be a source of big problem
Stay tuned as the event unfurls
Wednesday, February 29, 2012
Is the Sun really heading for Solar Maximum?

Akshay Deoras
Severe Earth & Space Weather Forecaster,Astrophysics article writer.www.scribd.com/akshaydeoras
Web-
www.akshaydeoras.blogspot.com
www.metdweather.blogspot.com
Tuesday, February 14, 2012
Static Instability
While seeing the weatherman said "It gonna be rain in Jakarta tomorrow", a critical person should think what mechanism driving the air to put down some of it moisture. He would run for YouTube, chasing the lapse rate videos showing the grow of cloud over time. Then he could also run for satellite images seeing the case of it. Then he would got a simple conclusion that the water vapor rises high to the sky and it cools down, and after that it rains. Then he asked again to himself, how a cloud could rise? Why not all cloud rising and pour rain? Then he may google it up and found articles talking about it. Some articles said that convective energy available in a specific area governs that. It may say that convective energy, is related to static instability.
Here, i just trying to talk about static instability. In meteorology, especially the one talking about weather phenomenon happening at the spatial scale of 2 - 2000 km (mesoscale), there are 5 types of instability: Static instability, Inertial instability, Shear instability, Symmetric instability, and Centrifugal instability. Each type of instability has their own use. The static instability is used to determine whether a place is potential for thunderstorm buildup or no. Even in tornadogenesis, static instability plays a great role in determining how powerful the tornado will be.
Formulation of Buoyancy
Let we consider a piece of air parcel trying to rise in the sky. The vector working at this air parcel is buoyancy B defined as these. \[\overrightarrow B = \overrightarrow g \cdot \frac{{\left( {T - \overline T } \right)}}{{\overline T }}\] For sure, because of buoyancy, the parcel of air is rising. Let's see that Newton's Law stated a force has acceleration, so then we can infer that the buoyancy force accelerates the air parcel upward against gravitational force, $\overrightarrow B = \frac{{d\overrightarrow w }}{{dt}}$, $\overrightarrow w$ is upward velocity. We also know that the upward velocity $\overrightarrow w = \frac{{d\overrightarrow {\Delta z} }}{{dt}}$ for ${\overrightarrow {\Delta z} }$ is displacement along the troposphere's depth. Then, we could describe the buoyancy force in more intricating form like these. \[\frac{{{d^2}\overrightarrow {\Delta z} }}{{d{t^2}}} = g \cdot \frac{{\left( {T - \overline T } \right)}}{{\overline T }}\] Now its the time to talk about the two kinds of T in equation above. The $T$ stands for air parcel temperature and the $\overline T $ stands for environmental temperature.
Breaking Apart the $T$ and $\overline T $
In meteorology, the $T$ and $\overline T $ are actually changing with height. We usually says that temperature decreases with height, but let us change that view: in case of air inversion caused when hot air is advected to a cooler region, air aloft is warmer than that of surface, so we better describe temperature as a continuous function of z; $T\left( z \right)$ and $\overline T \left( z \right)$. Then, if we fly from height z0 to height a in troposphere,
- \[T\left( a \right) - T\left( z_0 \right) = \int\limits_{{z_0}}^a {T'\left( z \right)dz} \]
- \[\overline T \left( a \right) - \overline T \left( z_0 \right) = \int\limits_{{z_0}}^a {\overline T '\left( z \right)dz} \]
- \[T\left( a \right) - T\left( {{z_0}} \right) = T'\left( z_0 \right)\left( {a - {z_0}} \right) + \int\limits_{{z_0}}^a {\left( {a - z} \right)T''\left( z \right)dz} \]
- \[\overline T \left( a \right) - \overline T \left( {{z_0}} \right) = \overline T '\left( z_0 \right)\left( {a - z_0} \right) + \int\limits_{{z_0}}^a {\left( {a - {z}} \right)\overline T ''\left( z \right)dz} \]
- Temperature of air parcel at height a
\[T\left( a \right) = T\left( {{z_0}} \right) + T'\left( {{z_0}} \right)\left( {a - {z_0}} \right) + ... + \frac{{{T^n}\left( {{z_0}} \right)}}{{n!}}{\left( {a - {z_0}} \right)^n}\] - Temperature of environment at height a
\[\overline T \left( a \right) = \overline T \left( {{z_0}} \right) + \overline T '\left( {{z_0}} \right)\left( {a - {z_0}} \right) + ... + \frac{{{{\overline T }^n}\left( {{z_0}} \right)}}{{n!}}{\left( {a - {z_0}} \right)^n}\]
${\Gamma _p} = T'\left( z_0 \right) \to \frac{{\partial T}}{{\partial z}}$, the change of air parcel temperature with the change of height and
$\gamma = \overline {T} '\left( {z_0} \right) \to \frac{{\partial \overline T }}{{\partial z}}$, the change of environmental air temperature as the height changes, so $T$ and $\overline T $ equals to:
- \[T = {T_0} + {\Gamma _p}\left( {\Delta z} \right)\]
- \[\overline T = {\overline T _0} + \gamma \left( {\Delta z} \right)\]
The first state of air parcel in atmosphere is always equilibrum, means that air parcel temperature is the same with environmental temperature (${T_0} = {\overline T _0}$), so that equation (7.) and (8.) finally become:
- \[T = {T_0} + {\Gamma _p}\left( {\Delta z} \right)\]
- \[\overline T = {T _0} + \gamma \left( {\Delta z} \right)\]
Stability of Environmental Lapse Rate
Reviewing the equation for $\overrightarrow B$, let us analyze it in depth.
- \[\overrightarrow B = \overrightarrow g \cdot \frac{{\left( {T - \overline T } \right)}}{{\overline T }}\]
- \[\frac{{{d^2}\overrightarrow {\Delta z} }}{{d{t^2}}} = \overrightarrow g \frac{{\left( {{T_0} - {\Gamma _p} \cdot \Delta z - {T_0} + \gamma \cdot \Delta z} \right)}}{{{T_0} - \gamma \cdot \Delta z}}\]
- \[\frac{{{d^2}\overrightarrow {\Delta z} }}{{d{t^2}}} = - \overrightarrow g \Delta z\frac{{\left( {{\Gamma _p} - \gamma } \right)}}{{{T_0} - \gamma \cdot \Delta z}}\]
- \[\frac{{{d^2}\overrightarrow {\Delta z} }}{{d{t^2}}} + \overrightarrow g \Delta x\frac{{\left( {{\Gamma _p} - \gamma } \right)}}{{{T_0}}} = 0\]
- \[\Delta z\left( t \right) = {C_1} \cdot {e^{i{{\left[ {{\textstyle{g \over {{T_0}}}}\left( {{\Gamma _p} - \gamma } \right)} \right]}^{\frac{1}{2}}}t}} + {C_2} \cdot {e^{ - i{{\left[ {{\textstyle{g \over {{T_0}}}}\left( {{\Gamma _p} - \gamma } \right)} \right]}^{\frac{1}{2}}}t}}\]
$C_1$ and $C_2$ is a constant depending on the magnitude and direction of initial parcel displacement. We don't use vector here because we emphasize the quantity of the vector as a function of time.
After changing the equation (15.) into complex form and taking just the real part, then we obtain this very (16.) equation.
- \[\Delta z\left( t \right) = \left( {{C_1} + {C_2}} \right) \cdot \cos \left\{ {{{\left[ {{\textstyle{g \over {{T_0}}}}\left( {{\Gamma _p} - \gamma } \right)} \right]}^{{\textstyle{1 \over 2}}}}t} \right\}\]
If ${\Gamma _p}<{\gamma }$, then $i{\left[ {{\textstyle{g \over {{T_0}}}}\left( {{\Gamma _p} - \gamma } \right)} \right]^{{\textstyle{1 \over 2}}}}$ becomes real. When the t is very big, the C1 can be ignored, and the equation would be like this.
- \[\Delta z\left( t \right) = {C_2}{e^{{{\left[ {{\textstyle{g \over {{T_0}}}}\left( {\gamma - {\Gamma _p}} \right)} \right]}^{{\textstyle{1 \over 2}}}}t}}\]
Convective Available Potential Energy (CAPE)
From the buoyancy equation above, an air parcel can only rise automatically if the temperature of air parcel is warmer than the environmental temperature. The level where the air parcel becomes warmer than the environmental temperature is called Level of Free Convection or LFC. Other point important in determining CAPE is equilibrum level, is when the air parcel temperature cools down to be the same with environmental temperature again.
This is the skew-T log-P plot showing CAPE, level of free convection, and equilibrum level.
Deriving CAPE:
- \[\frac{{d\overrightarrow w }}{{dt}} = \overrightarrow B \]
- Multiplying (18.) with $\overrightarrow w \equiv \frac{{d\overrightarrow z }}{{dt}}$
\[\overrightarrow w \frac{{d\overrightarrow w }}{{dt}} = \overrightarrow B \frac{{d\overrightarrow z }}{{dt}}\] - \[\frac{d}{{dt}}\left( {\frac{{{{\overrightarrow w }^2}}}{2}} \right) = \overrightarrow B \frac{{d\overrightarrow z }}{{dt}}\]
- Canceling the $dt$, and integrating (20.) from LFC from EL.
\[\int\limits_{LFC}^{EL} {d{{\overrightarrow w }^2}} = 2\int\limits_{LFC}^{EL} {\overrightarrow B \cdot d\overrightarrow z } \] - Vector dot product is scalar. So then,
\[w_{EL}^2 - w_{LFC}^2 = 2\left[ {CAPE} \right]\] - Since the vertical velocity $w$ at level of free convection equals 0, so vertical velocity at equilibrum level is considered maximum. Then,
\[w_{EL}^2 = 2\left[ {CAPE} \right]\] - \[\frac{1}{2} \cdot w_{EL}^2 = CAPE\]
Putting All Above Together
What drive cloud to pour rain? It is instability. Instability is driven by difference between air parcel temperature and environmental temperature. The more moisture an air parcel has, its lapse rate would be smaller (remember that water vapor is a good heat storage). Also, sky above a suburb or city is normally has bigger lapse rate compared to a field or forest. Steep lapse rate also experienced in frontal boundary. In mountains, the environmental lapse rate experienced there is a mix between horizontal and vertical environmental lapse rate, and that two are always big there. Big lapse rate of environment added with small lapse rate of air parcel would make the air parcel rise. The rising air parcel cools into water dropplet or ice (if the buoyancy is great), graupel or snow (if buoyancy is just positive). A tremendous buoyancy will turn the air parcels into a tremendous castle of cumulonimbus cloud - that's why forecasters uses CAPE as a parameter for determining thunderstorm. Buoyancy can even tilt a horizontally aligned rotational motion of air into an EF-5 wedge tornado. The buoyancy of air parcel in sea is relatively smaller than that of land (except in equator where the air parcel is forcedly lifted), because the environmental lapse rate is small, and so does the parcel lapse rate. In desert, the air parcel is mostly dry, so its lapse rate is big, along with the environmental lapse rate. What about hurricane forming in the sea? It is the case of shear instability, that later turned on the static instability and moreover, the inertial instability. Not all cloud pouring rain, because:
- Clouds have different rate of inner instability depending on their origin. The most unstable one will perform convection and possible to pour rain.
- The environmental lapse rate should be adequate to fire convection if no cloud is sufficiently unstable.
Wednesday, February 8, 2012
Prime numbers
-ALUTSYAH LUTHFIAN-
Tuesday, January 24, 2012
Geomagnetic Sudden Impulse! CME arrives earlier than SSW forecast
AKSHAY DEORAS
SEVERE WEATHER FORECASTER
THE CME FROM THE JAN 23RD SOLAR FLARE HAS ARRIVED AND HAS CAUSED A GEOMAGNETIC SUDDEN IMPULSE.
STAY TUNED FOR MORE UPDATES!
Akshay Deoras
www.akshaydeoras.blogspot.com
www.metdweather.blogspot.com
Major Geomagnetic Storming expected due to CME of M9 class flare
Akshay Deoras
Severe Weather Forecaster
A MAJOR GEOMAGNETIC STORMING IS LIKELY FROM TONIGHT ( GMT) OVER 25TH JAN 2012
The Mega-flare of January 23rd, which released massive and very very fast moving CME towards the Earth is expected to cause a Major Geomagnetic Storming. Initial estimates from the Goddard Space Flight Center confirm that the CME speed was over 2200km/sec when released !
The arriving models are confirming that the CME is Earth-directed and likely to hit the Earth's Magnetic Field on night hours of 24th Jan 2012 today ( GMT).
As the momentum of CME is very high, it will definitely give a very strong hit to the Earth's magnetic field which definitely will trigger Major Geomagnetic Storm
The estimates are suggesting that the Geomagnetic Storming level can reach upto G3 level which the Space Weather Prediction Center of NOAA also suggests.
Attached below is the model which shows the approaching CME
Below model image shows CME just before the impact-
Highlights-
A VERY STRONG CME IS HEADING TOWARDS THE EARTH AND WILL HIT THE EARTH'S MAGNETIC FIELD ON NIGHT HOURS ( GMT) OF 24TH JAN 2012
* A MODERATE TO STRONG GEOMAGNETIC STORM UPTO G3 LEVEL IS EXPECTED DUE TO IT
* THE FLIGHTS TRAVELLING IN POLAR ORBIT ( POLAR ROUTE) WERE EXPECTED TO MAKE A PATH CHANGE TO AVOID EXPOSURE TO RADIATION!
* THE CME WILL SPARKLE AURORAS IN HIGH LATITUDE AND LIKELY IN LOW LATITUDE AREAS ALSO.
STAY TUNED FOR UPDATES @
http://www.facebook.com/pages/Severe-Solar-Weather-forecast/112556765473804
Monday, January 23, 2012
M9 Class Solar Flare with CME released towards the Earth
monitor the situation LIVE
HERE
Update-
0520hrs UTC,23rd Jan 2012
The Solar Flare has been recorded as an M9 or the last level of the M class flare! Coronal Mass Ejection has taken place which is heading towards the earth due to the geo-effective position. The source of this Solar flare seems to be the region AR 1402 and not the AR 1401
STAY TUNED FOR UPDATES
Saturday, January 21, 2012
Moderate Geomagnetic Storming possible ahead of CME release from M3 Solar Flare
Akshay Deoras
Severe Weather Forecaster
The nearly quiet space weather has activated after a brief gap considering the 1-Month ( Dec 2011) avg sunspot number to be less ( decreased value) after Nov 2011 as per Solar IPS.The observed no is 73.0 as against the predicted of ~ 72 for Dec 2011
Saturday, December 10, 2011
MOON IN THE PENUMBRAL PHASE IN NAGPUR
Akshay Deoraswww.scribd.com/akshaydeoras
Severe Earth & Space Weather Forecaster,Astrophysics article writer.
Web-
www.akshaydeoras.blogspot.com
www.metdweather.blogspot.com
AKG SETUP FOR THE LUNAR ECLIPSE
Akshay Deoras
Severe Earth & Space Weather Forecaster,Astrophysics article writer.
Web-
www.akshaydeoras.blogspot.com
www.metdweather.blogspot.comwww.scribd.com/akshaydeoras
Total Lunar Eclipse today!
The MOST AWAITED TOTAL LUNAR ECLIPSE IS TODAY
As known by all, the second total lunar eclipse will start today with the penumbral phase at around 1133UT.
AKG Networks will BE PASTING REAL TIME PHOTOS ON OUR BLOGS-
www.akshaydeoras.blogspot.com
www.metdweather.blogspot.com
www.rajesh26.blogspot.com
twitter.com/lunarakg
facebook.com/deorasakshay
AND WE ARE PROUD TO ANNOUNCE A TIE UP WITH VAGARIES OF WEATHER -
www.rajesh26.blogspot.com WHERE THREE IMPORTANT PHOTOS WILL BE PASTED AT 1330UT,1430UT AND 1530UT. THOSE WHO WILL NOT BE ABLE TO SEE THE LUNAR ECLIPSE ARE ENCOURAGED TO MONITOR IT ON AKG NETWORKS BY FOLLOWING REAL TIME TWEETS ON twitter.com/lunarakg
THE LIVE COVERAGE WILL BEGIN TODAY AT 1130UT ON TWITTER AND BLOG
OTHER LIVE STREAMERS
1] Hong Kong Observatory- SEE HERE ( Coverage begins at 0845PM LT)
2] Siliguri,India SEE HERE ( Coverage begins 1230UT)
3] Star Gazers SEE HERE
4] astronomylive.com
FOR AKG NETWORKS PHOTO,MEDIA PERSONS MUST CONTACT AT
akshaydeoras@hotmail.com
Thursday, December 8, 2011
More FAQ about Lunar Eclipse
Q. For the regions shown ( Eclipse at Moon rise) in the above figure what will happen?
A. People are confused about Eclipse and Moonrise of this Saturday's. Well, for the regions in the Eclipse at Moonrise the exact meaning is that the lunar eclipse ( already in progress) will be seen after the moon rises. Lets think of a simple example.
Consider a train ( moon) travelling from station A( Regions where all eclipse will be visible) to station B ( regions of Eclipse at Moonrise). An observer will say that the eclipse has begun when he sees the train at either of the station. That is observer at station A will see the train first and shortly the eclipse will begin ( Passengers board the train) but for the observer at B station, the train ( Moon) and passengers ( Eclipse) isn't visible! Lets think that the train arrives at a certain time. Thus ONLY AFTER THIS TIME( Moonrise) the person will see the train ( moon) and passengers ( eclipse) and such will be the situation.
For much of India, the lunar eclipse Penumbral phase w'd have begun before but will be visible only after the moon arrives.
Q. Eclipse starts at 0615PM IST in India.What does it mean when you say eclipse begins at moonrise?
A.The time 0615PM IST is the time when the Partal Lunar Eclipse will begin.Infact the penumbral eclipse starts much before the moon rise.
Q. What can one see through unaided,untrained eyes during the penumbral eclipse phase?
A.The penumbral eclipse actually takes place when the moon enters the penumbra ( Outer light shadow of the earth.) For untrained,unaided eye not much change will be there. One will keep seeing the moon without any change in its geometry however the moon shall dim a bit ( if observed properly).
Q. Terminologies Partial,Umbra,Penumbra,Totality are confusing.How can it be made simple?
A. Its very easy!
The Earth's shadow is of the circular form. Consider the below Dart-Board
The outer circle where numbers are written is the Penumbra of earth's shadow ( Lighter shadow region)
The inner circle is the Umbra of earth's shadow ( Darker region).
The Moon in the numbered circular region is said to be in Penumbral Eclipse.
But when the moon enters inside and moves in the inner circular region ( COMPLETELY) then its said to be in Totality..
A Partial Lunar Eclipse will occur when some part of the moon enters the inner circular region but most of the moon is outside it.
Q. How will the moon look at what time on 10th Dec 2011?
A.There is a wonderful link on it. See here
Q. How long will the Lunar Eclipse of 10th Dec 2011 last?
The totality phase shall last till around 51mins i.e one will be able to observe the darker shade of Moon with the Brick Red or copper red shade.
The rest eclipse ( Penumbral to Penumbral) will last close to 6 hours!
Tuesday, December 6, 2011
Expected weather forecast for Lunar Eclipse 10th Dec 2011
Akshay Deoraswww.scribd.com/akshaydeoras
Severe Earth & Space Weather Forecaster,Astrophysics article writer.
Web-
www.akshaydeoras.blogspot.com
www.metdweather.blogspot.com
Friday, December 2, 2011
"Science of Lunar Eclipse through FAQ & Celestial Beauty of Saturday"
The coming Saturday,10th Dec is going to be a wonderful evening for all the astro lovers! There will be a Total Lunar Eclipse on the evening of Saturday which will be the second one of the year ( After 15th June 2011) when the first total lunar eclipse was seen.
The Myth of Eclipses
The phenomena of eclipse wasn't as enjoyable thousands of years ago as it is today especially to see the copper red moon of totality.
For those who don't know the science of the eclipse, lets learn it through Frequently Asked Questions (FAQ)Chinese people had mentioned first about Solar Eclipse long way back around 2134BC. People of the ancient times used to fear from the eclipse as they thought it was a curse. Even the famous war between Lydians and Medes ended after 5 years at once as the day turned dark due to Solar Eclipse- A phenomena which they didn't understand.
Lunar Eclipse occurs when the Earth's shadow falls on the moon.When I am standing in front of a tube light my shadow falls behind ( Say there is a screen). This screen is the moon and I am the earth for consideration
Q.How is the moon's orbit around the Earth?A.The orbit of the moon around the Earth is an ellipse ( curve obtained when you join letter "u" from top with inverted "u"). Moon's orbit around the earth makes an angle of 5 Degree 14 mins with the ecliptic ( Ecliptic plane is the plane in which Earth orbit's the Sun)Its like when you consider a clock let the minute hand pointing from 9 to 3 be ecliptic. So the second's hand pointing from 10-4 and 8-2 is the moon's orbit around the earth but in the real three dimension of space.
Thus the second's hand crosses the plane two times.At 9'o clock and 3'o clock.The same is the concept of Moon.
Moon's orbit crosses the ecliptic two times during one orbit referred as nodes( Explained below)Thus for earth's shadow to be casted on moon or moon blocking the solar disc, the moon must be in a common plane with earth and sun i.e have co-planar orbits.
Q. When Moon crosses the ecliptic twice a month, then why there isn't eclipse twice a month?
A. Consider the below figure

L = 0 Very dark eclipse.Moon almost invisible, especially at mid-totality.
L = 1 Dark Eclipse, gray or brownish in coloration. Details distinguishable only with difficulty.
L = 2 Deep red or rust-colored eclipse. Very dark central shadow, while outer edge of umbra is relatively bright.
L = 3 Brick-red eclipse.Umbral shadow usually has a bright or yellow rim.
L = 4 Very bright copper-red or orange eclipse.Umbral shadow has a bluish, very bright rim.
Friday, November 18, 2011
My Ordinary Opinion about Multiverse

When the electricity went down in my area, i think of this: In the darkness, I feel that every movement I made is always in positive magnitude, since i don't know to where i go (if i ignore my own sense of "going back", "going front", and "going upward" and also "going downward"). This could be applied to time: we are all plunged in the darkness of time.
After that, I thought that this universe has maximum 7 dimension, with the first 3 dimensions are related to the properties of physical things, and the next 3 dimensions are related to time, in which we can't feel its presence.
The uppermost 1 dimension is related to the position of the Supreme Being whose control the all 6 dimensions below Him.
That's it, this is only my opinion.
Friday, October 28, 2011
Earthquake in Turkey

Sunday, October 23, 2011
Strong Earthquake hits Turkey.. The intensity map shows intensity 9 damage near Van,Turkey
Akshay Deoras
www.akshaydeoras.blogspot.com
www.metdweather.blogspot.com





















