Thursday, September 30, 2010
Arabian Sea ‘low' sustains peninsular rains
Wednesday, September 29, 2010
Monsoon withdraws from more parts of North-West India
South-West monsoon has withdrawn from some parts of Punjab, Haryana, Rajasthan and Gujarat on Monday in what looks like the precursor to an unusually rapid exit from the entire upper half of mainland India.
The hurried withdrawal is being attributed to its ‘release' from a temporary pause enforced around September 16 half way to the east by contra-indicating weather systems.
WEATHER INTERACTION
This was the phase when the build-up to withdrawal ran itself up against hyperactive interaction between a deep-seated trough in the western disturbance with easterlies from the Bay of Bengal triggering torrential rains over Uttarakhand, Haryana and Delhi.
After the interaction spent itself out, the way has become clear for the dry westerly-to-northwesterlies to push into these areas and expedite the withdrawal process all over again.
An India Meteorological Department (IMD) update on Monday said that the withdrawal line passed through Amritsar, Hissar, Jaipur, Udaipur, Ahmedabad and Porbandar.
MORE COVERAGE
Conditions are favourable for further withdrawal from remaining parts of Punjab, Haryana, Delhi, Chandigarh, Rajasthan, Gujarat, Jammu and Kashmir, Himachal Pradesh and Uttarakhand and even parts of Uttar Pradesh and Madhya Pradesh during the next two to three days.
Satellite picture also indicated drying up of moist air over parts of North-West India, the IMD update said.
But the weather being set up in peninsular India by active circulations in the Bay of Bengal and the Arabian Sea could keep the withdrawing monsoon at bay for the time being.
CONVECTIVE CLOUDS
Satellite pictures revealed the presence of convective clouds over parts of Arunachal Pradesh, Meghalaya, Tamil Nadu, North Orissa, South Chhattisgarh, South Konkan, Goa, South Peninsular India, East-Central and South Bay of Bengal, Andaman Sea and East-Central and South-East Arabian Sea. The IMD update said that during the last 24 hours ended Monday morning, widespread rainfall was reported from North Konkan, Goa and Coastal Karnataka.
It was fairly widespread over the Northeastern States, Madhya Maharashtra, Interior Karnataka, Kerala and Tamil Nadu while being scattered over Sub-Himalayan West Bengal, Sikkim, South Gangetic West Bengal and Lakshadweep.
The cyclonic circulation over Lakshadweep persisted from overnight.
SOUTH BAY WHIRL
International weather models suggested that occasionally wet weather would prevail over South Peninsular India until October 13, with another weather system forecast to take shape off South-East Tamil Nadu coast and just to the NorthEast of Sri Lanka.
The European Centre for Medium-Range Weather Forecasts (ECMWF) has predicted that a western disturbance could make its presence felt over the plains of North-West India by October 6.
This would be followed the very next day by the formation of a cyclonic circulation off South-East Tamil Nadu coast. It remains to be seen whether this could in fact mean the onset of the retreat monsoon (North-East or winter monsoon) over the peninsula.
In extended forecasts, the US National Centre for Environment Prediction (NCEP) sees this system driving rains across Tamil Nadu and Kerala as well as over parts of Karnataka and South Andhra Pradesh during the week ending October 13.
Meanwhile, an IMD weather outlook valid until Thursday said that fairly widespread rain or thundershowers would occur over Sub-Himalayan West Bengal, Sikkim, the North-Eastern States, Konkan, Goa, Tamil Nadu, Karnataka, Kerala, Lakshadweep and Andaman and Nicobar Islands.
They would be scattered over Interior Maharashtra, Andhra Pradesh, Orissa, Gangetic West Bengal and South Chhattisgarh.
But mainly dry weather would prevail over plains of North-West India, Bihar, Madhya Pradesh and Jharkhand indicating likely withdrawal of monsoon from these areas.
Extended forecast valid until Saturday said that fairly widespread rainfall would occur over South Peninsular India while rains would dry up over North-East India as well.
Climate Scam: NGO credibility hit a new low. The shame much worse than their Rwandan Genocide culpability
We as member of the NGO fraternity or general public seldom research their record of accomplishment; or ask awkward questions on northern NGOs policies; or chase facts behind their claims and publicity spin. One of the most basic questions as we dig deeper is what kind of credentials do these northern NGOs possess to champion justice issues. Simply put - are they committed to principles of justice as portrayed in their carefully cultivated public image?
If we go back to history, what we find is that they have a chequered past in terms of justice credentials. Rwandan Genocide until now had been regarded as the worst shame of NGO behaviour. This was genocide where an estimated 800,000 were massacred. The nineties saw NGOs soul-searching on such behaviour even as today NGO workers remain mentally scarred of experiences such as Rwanda. Apparently lessons have not been learnt as we find that through their climate advocacy they have not only repeating the mistakes of the past but the shame hit a new low.
Read more: http://devconsultancygroup.blogspot.com/2010/09/climate-scam-ngo-credibility-hit-new.html
S. Arabian sea system .. "92A"... update # 1
Here's the satellite shot of the Arabian sea system.
and latest IR shot of the potential system.
Numeric models predict... that the system will slightly move North, then die down and followed by another LOW circulation almost immediately in the same S. Arabian sea zone.
The present and next low level circulation is expected to persist well into 6-Oct-2010.
NO cyclone or depression formation is seen from the system.
NO north ward movement into Arabian sea is also not predicted.
Tuesday, September 28, 2010
Monday, September 27, 2010
Sunday, September 26, 2010
Places which has received nearly 400 cm for the year
- Cherrapunji (Meghalaya) - 1278 cm (Annual around 1100)
- Agumbe (Karnataka) - 638 cm (Annual over 750)
- Gaganbawada (Maharashtra) - 540 cm (Annual over 600)
- Mahabaleshwar (Maharashtra) - 431 cm (Annual over 600)
- Shirali (Karnataka) - 430 cm (Annual over 400)
- Passighat (Arunachal Pradesh) - 419 cm (Annual around 450)
- Coochbehar (West Bengal) - 417 cm (Annual around 350)
- Silchar (Assam) - 417 cm (Annual around 350)
- Buxa (West Bengal) - 405 cm (Annual around 550)
- Mangalore AP (Karnataka) - 397 cm (Annual around 400)
- Harnai (Maharashtra) - 396 cm (Annual around 250)
- Panambur (Karnataka) - 393 cm (Annual over 350)
- Bhagamandala (Karnataka) - 384 cm (Annual over 600)
- Honavar (Karnataka) - 383 (Annual over 350)
- North Lakhimpur (Assam) - 376 cm (Annual around 350)
- Kottigehara (Karnataka) - 375 cm (Annual around ??)
Saturday, September 25, 2010
Maharashtra begins artificial rain project
Why the jubilation then? Because these regions fall within 10 most scarcity-hit districts of Maharashtra with no rains for the last three years. The state government has imported the requisite radar machines and other equipment at a cost of Rs.5.5 crore and hopes to continue creating artificial ‘November rains’ equipped with a Piper Cheyenne plane (light aircraft), armed with hygroscopic salts, for cloud seeding sorties over these and other scarcity hit regions.
Chief minister Sushilkumar Shinde said today: “The artificial rain is the outcome of an agreement signed between the state government and Ms Weather Modification Co through its subsidiary Ms Agni Aviation Consultants (Bangalore) on August 21, 2003. The equipment was imported and became operational on Saturday with the first experiment resulting in 11 mm of rainfall experienced over a 12 square km patch in Satara district for 31 minutes. The next day (Sunday) the same experiment was repeated in the three rural regions where around 6.5 mm of rainfall was recorded.
Source: Business Standard
Rains this season create records in Mumbai, Delhi, Jaipur & Dehradun
Mumbai - breaking 50 year record
Monsoon has created a record of sorts this year. The rainfall witnessed is well on course to be ranked as the highest ever recorded in the city. There have been a number of intense rain spells, yet the city life has not been thrown out of gear even once. The data of monsoon witnessed between 1999 and 2009 indicates that there had been at least two rain days every year when the city life was halted, a senior official from the civic disaster management cell said. The Santa Cruz observatory has witnessed 3,309.2 mm rain this year, while the Colaba observatory has received 3,160.5 mm. A Met department officer said that with there being still some time before the monsoon withdraws, the rainfall-recorded is on course to be the highest ever. According to a senior official, the Santa Cruz observatory had recorded about 3,400mm rainfall in 2005, the year when an unprecedented rain event on July 26 saw a downpour of 944 mm. The second-highest rainfall recorded by the suburban observatory was 3,281.7 mm in 1958. The Met officials also suggested that the Colaba rainfall has already surpassed all rain records set in the past 50 years.
The monsoon rainfall broke a 44-year-old record in Dehra Dun by registering a whopping 3088 mm of rainfall this season. Met Director Anand Sharma told PTI that the previous highest record was in 1966 when the Doon valley recorded 2930 mm of rainfall. Before 1966, records regarding monsoon rains are not available, he said. With heavy rains lashing Dehra Dun, several rivers in the valley were on spate which include Rispana, Bindal and Asan. Nine of the total 13 districts of Uttarakhand have received excess rainfall this monsoon season.
Jaipur - breaking 14 year record
Breaking a 14-year record, Jaipur received 781.2mm rain this year till Wednesday. Going by the Met department’s prediction, as the monsoon is still active in the state and will last till the end of the month, the figure is likely to change in the coming few days. According to officials of Indian Meteorological Department, Jaipur receives around 500 mm rainfall in normal circumstances. The last time it had rained so much was in 1996, when the showers had been plentiful to the point of becoming an abnormality. Jaipur city had then received 850 mm rain between June and September. Looking at the conditions of this year, Jaipur is heading towards and abnormal spell of monsoon. "The district has already received 40% rain in excess of the normal this year," an irrigation official said. The comparison becomes obvious with last year's rainfall chart when Jaipur received less than 300 mm rain and had to be included among the scarcity-hit districts of the state.
Delhi - breaking 32 year record
Records shows this is the wettest monsoon in Delhi since 1978. Rainfall since June 1 has touched 1004mm higher than 965.1mm recorded during the monsoon of 1978. Sunday's rain also took Delhi's rainfall during September to 250.6mm, the highest since 1998 when 280.4 mm was recorded. Last year, the figure had settled at 588 mm. Delhi recorded 455.1 mm rain in August, more than double its normal average of 225.8 mm. With 10 days remaining in the month, September too is poised to break records having recorded around 280mm more than normal.
LA NINA & NEM 2010
La Niña strengthened during August 2010, as negative sea surface temperature (SST) anomalies reached at least -1oC across most of the equatorial Pacific Ocean by the end of the month. Consistent with this evolution, the subsurface heat content (average temperatures in the upper 300m of the ocean) decreased further, reflecting the additional cooling of sub-surface waters east of the International Date Line.. Also convection was enhanced over Indonesia, while remaining suppressed over the western and central equatorial Pacific. The pattern was associated with the continuation of enhanced low-level easterly trade winds and anomalous upper-level westerly winds over the western and central equatorial Pacific. Collectively, these oceanic and atmospheric anomalies reflect the strengthening of La Niña.
- During last week the equinoctial Pacific SST have been NEGATIVE:
- LA NINA is expected to last during this Northern Hemisphere winter [2010-11]
- Though Indonesian region convective activity is expected to enhance, sleek of this convective belt into Bay is NOT predicted.
- There is chance that cold tongue may cross and sleek into western Pacific unto Indonesia.
Courtesy: Climate Prediction Center / NCEP
20 September 2010 {update}
Friday, September 24, 2010
Thursday, September 23, 2010
MONSOON TAIL
Wednesday, September 22, 2010
Es Safa Volcanic Field, Syria
Es Safa is a striking basaltic volcanic field located to the southeast of Damascus, Syria. It lies within the larger Harrat Ash Shamah—the largest volcanic field on the Arabian tectonic plate. Harrat Ash Shamah parallels the Red Sea and extends from northeastern Israel, through southern Syria and Jordan, and into Saudi Arabia, covering an area of over 50,000 square kilometers (19,000 square miles).
Es Safa contains numerous vents that have been active during the Holocene Epoch (beginning approximately 12,000 years ago). The most recent recorded activity was a boiling lava lake observed in the area around 1850. The dark lava flow field (center) likely represents the latest activity of the volcanic field, and is emplaced over older, lighter colored flows. The older flow surfaces also have light tan sediment accumulating in shallow depressions, in contrast to the relatively pristine surfaces of the darker, younger flows.
Cinder cones are scattered throughout the Es Safa field, but many are aligned along northwest-southeast trends that likely indicate faults through which magma rose to the surface. Two such alignments are visible at image left. To the southeast (image right) a small reservoir feeds water distribution ditches extending northwards.
La Nina in progress
Continuing a trend that began earlier in the year, La Niña conditions strengthened through the summer of 2010, evidenced by a streak of cool water across the equatorial Pacific Ocean.
Acquired by the Ocean Surface Topography Mission/Jason-2 satellite, this map shows a 10-day average of sea-surface height centered on September 6, 2010. Because water expands with rising temperatures, satellites can use sea-surface height as a proxy for temperature. Areas where the water surface is higher (and therefore warmer) than average are shades of red-brown, and areas where the water surface is lower (cooler) than average are blue. Normal conditions appear in white.
The El Niño weakens the westward trade winds that normally blow over the eastern tropical Pacific Ocean. Those winds keep eastern Pacific waters cool and concentrate warm waters in the western Pacific. A weakening of trade winds enables warm waters to gradually spread eastward, heating up the central Pacific. La Niña typically follows El Niño, and causes essentially the opposite conditions. La Niña strengthens the trade winds, spreading cool water from the South American coast to the central Pacific. This see-saw pattern of El Niño and La Niña can drive large-scale weather changes, especially in the tropics.
This map reveals a broad swath of cool water stretching from South America to New Guinea. The ocean is not, however, uniformly cool. Pockets of warm water are mixed with the cool, particularly in the western Pacific. Warmer waters in this region can lead to increased rainfall, and La Niña conditions may have played a role in the devastating floods in Pakistan during the Northern Hemisphere summer of 2010.
Over the eastern Pacific Ocean, cooler waters lead to less moisture along the coasts of North and South America. So as more rain pounds some parts of the globe, La Niña conditions can deepen drought in others. By the time La Niña conditions intensified in September 2010, the southwestern United States had experienced more than 10 years of mostly dry conditions. A release from NASA’s Jet Propulsion Laboratory reported that the American Southwest might experience not only drier conditions, but also intensified wildfires under strong La Niña conditions.
OSTM/Jason-2 is a joint oceanographic mission of NASA and the Centre National d’Études Spatiales (CNES), France’s space agency.
Tuesday, September 21, 2010
10 tell tale signs that the global warming is a dying hoax.
1. Re-branding exercises
Read more: http://devconsultancygroup.blogspot.com/2010/09/for-climate-justice-activists-living-in.html
Monday, September 20, 2010
Only 40% North East Monsoon rainfall for Tamilnadu - 2010
But I am very pessimistic about NEM 2010 rainfall. It is and it will be a "RETREATING" SW monsoon with [I hope] lesser than normal rainfall. LA NINA will be stronger during Oct Nov Dec 2010 and cold tongue will be penetrating from East central Pacific to Western Pacific to Indian Ocean and some time may bring colder than normal minimum temperature in East coast especially SCAP & N-TN.
posted by Kaneyen
Overall rainfall improves to 103%
Sunday, September 19, 2010
Dehra Dun breaks a 44-year monsoon record by registering a whopping 3018.3 mm of rainfall this season
Saturday, September 18, 2010
Friday, September 17, 2010
Thursday, September 16, 2010
Wednesday, September 15, 2010
Hurricane Igor
Tropical Storm Igor formed over the far eastern tropical Atlantic Ocean on September 8, 2010, the U.S. National Hurricane Center (NHC) reported. From its genesis locality southeast of Cape Verde, Igor traveled westward. Igor strengthened to a hurricane on September 11, becoming the fourth of the season. By 11:00 a.m. Atlantic Standard Time (AST) on September 13, Igor was a category 4 hurricane, packing maximum sustained winds of 150 miles (240 kilometers) per hour.
The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite captured this natural-color image of Hurricane Igor at 12:40 p.m. AST (16:40 UTC) on September 13, 2010. Igor shows all the characteristics of a strong hurricane, including a distinct eye and spiral arms spanning hundreds of kilometers.
On September 13, the NHC forecast that Igor would continue moving toward the west at about 10 miles (17 kilometers) per hour. Late in the day on September 13, or early in the day on September 14, Igor was expected to turn toward the west-northwest. Although the storm’s intensity would likely fluctuate over the next 48 hours, it was expected to remain a powerful hurricane.
Landslide in Zhouqu, China
Tucked between the steep slopes of the Min Shan and the Bailong River in northwest China, the city of Zhouqu has a picturesque location. However, the intimidating natural beauty also carries a risk. On August 8, 2010, unusually intense monsoon rains triggered devastating landslides and floods that buried a densely populated area in the center of the city. As of August 17, China’s official news agency reported 1,270 deaths with 474 people still missing. This detailed image, from DigitalGlobe’s WorldView-2 satellite, shows the largest slide in the lower part of the city on August 10.
The slide terminates in a brown fan that extends into the Bailong River. Mud surrounds several of the buildings near the river’s edge and branches into adjacent streets. Some of this mud may have been deposited by flood waters that gathered behind the slide as torrential rain continued to fall. In the large image, which shows a wider area, the dark waters of Bailong River seeps around buildings across from the slide and up the wide road that runs along the river’s edge not far from the slide.
Moving away from the river, the mud has a rougher, more varied texture where the slide channeled through the center of the city. The smooth dark spots are probably water. Light-colored flecks are probably debris. The slide area widens again in the lower right corner, clearly covering blocks of buildings.
Slightly darker than the surrounding mud, streams snake across the surface of the slide. The large image reveals that the landslides followed the course of streams down the mountains and into the valley where Zhouqu was built. On the far right side of the large image, closer to the top of the slide and beyond the right edge of the web image, farmland surrounds the streams. The steep slopes on either side of the streams are bare of vegetation, possibly making them prone to landslides.
Following intense monsoon rains, a landslide struck Zhouqu County of China’s Gansu Province on August 8, 2010. By early September, the death toll stood at 1,765, Dave’s Landslide Blog reported, and this single event contributed to an unusually high worldwide death toll for landslides in 2010.
Weeks after the event, the landslide in remained visible to the Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite. ALI captured this natural-color image on September 2, 2010. Bare earth forms a giant Y shape on the otherwise forested mountain slopes. The separate slides have coalesced into a wide river of mud flowing into town. Clouds leave part of the landscape in shadow, but the landslide remains discernible all the way to the river at the bottom of the valley.