rain fall

The very severe cyclonic storm Sidr over the Bay of Bengal is expected to trigger heavy rainfall and cause high tides late Thursday in Orissa's four coastal districts meteorological officials said. 'The system moved further northwards Thursday and lay centred over east central and adjoining west central and north Bay of Bengal at about 350 km south east of Paradeep,' S. N. Gouda of the Bhubaneswar Meteorological Office told IANS. 'The system with maximum sustained go speed of 200 kmph is likely to go across the West Bengal-Bangladesh glide east of Sagar Island by Thursday midnight,' Gouda said. Rain or thundershower is likely to occur in most coastal areas with isolated extremely heavy rainfall in north Orissa causing floods in low lying areas. Under the cyclonic influence five to six metres high tidal waves are likely in coastal areas of Orissa's Balasore. Bhadrak. Kendrapara and Jagatsinghpur districts. Gale winds speeds reaching of 90-120 kmph are also likely to blow over the coastal areas from late Thursday the meteorological official said. Fishermen undergo been warned not to venture into the sea because it ordain remain prepare. The wind and rain may cause extensive damage to kutchha (mud) houses disruption of power and communication lines. It may also break complain and road traffic. Cautionary Signal number Three (LC-III) has been hoisted at Paradeep. Gopalpur. Chandbali and Puri ports. Gouda said. Chief Minster Naveen Patnaik has instructed the district administration of the eight coastal districts to be alert a state revenue official said.

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The very severe cyclonic storm Sidr over the Bay of Bengal is expected to trigger heavy rainfall and create high tides late Thursday in Orissa's four coastal districts meteorological officials said. 'The system moved advance northwards Thursday and lay centred over east central and adjoining west central and north Bay of Bengal at about 350 km south east of Paradeep,' S. N. Gouda of the Bhubaneswar Meteorological Office told IANS. 'The system with maximum sustained wind speed of 200 kmph is likely to go across the West Bengal-Bangladesh coast east of Sagar Island by Thursday midnight,' Gouda said. Rain or thundershower is likely to become in most coastal areas with isolated extremely heavy rainfall in north Orissa causing floods in low lying areas. Under the cyclonic influence five to six metres high tidal waves are likely in coastal areas of Orissa's Balasore. Bhadrak. Kendrapara and Jagatsinghpur districts. Gale winds speeds reaching of 90-120 kmph are also likely to blow over the coastal areas from late Thursday the meteorological official said. Fishermen undergo been warned not to venture into the sea because it will remain rough. The wind and rain may create extensive damage to kutchha (mud) houses disruption of cater and communication lines. It may also break rail and road traffic. Cautionary communicate be Three (LC-III) has been hoisted at Paradeep. Gopalpur. Chandbali and Puri ports. Gouda said. Chief Minster Naveen Patnaik has instructed the district administration of the eight coastal districts to remain alert a state revenue official said.

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Steve Bensen. The Carpetbagger inform. November 14. 2007 Following up an item from last week. Georgia is in the midst of an awful drought and express officials are running out of ideas to broach with the area’s water shortage. Georgia Gov. Sonny Perdue (R) responded by organizing a multi-denominational prayer function in which state officials and clergy would collectively ask The Man Upstairs to turn on the water works. Bowing his continue outside the Georgia Capitol on Tuesday. Gov. Sonny Perdue cut a newly repentant evaluate as he publicly prayed for rain to end the region’s historic drought. “Oh father we adjudge our wastefulness,” Perdue said. “But we’re doing better. And I thought it was measure to adjudge that to the creator the provider of water and land and to express him that we ordain do exceed.” Yes in the 21st century we undergo a state’s chief executive bargaining with God for rain. (The governor didn’t say. “If you give us rain we’ll be good,” but he came close.) Perdue implicitly conceded that the state has been negligent in its conservation efforts - his administration saw this coming but decided not to act more stringent conservation measures - but apparently wants God to furnish Georgia another chance. Perdue said after the event that Georgians have not done “all we could do in conservation” and that the drought was an attempt by God to “get our attention.” This entry is filed under. You can follow any responses to this entry through the cater. You can or from your own site. Oh ye of little faith! We had a drought here in the Holy State of California and a raindance was organized - an American Indian rain dance. Yes. Then it rained. Coincidence?You don’t experience for sure do you. GH it DID rain in GA! By now that may be the next day or somethin’ but it did rain. There would have been more rain had the American Indians been involved and had all athiests been unceremoniously escorted to the LA border.

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December 7. 2007 SMALLER STORMS DROP LARGER OVERALL RAINFALL IN HURRICANE toughen Researchers have found that when residents of the U. S southeastern states look skyward for rain to alleviate a long-term drought they should be hoping for a tropical storm over a hurricane for more reasons than one. According to a new chew over using NASA air data smaller tropical storms do more to alleviate droughts than hurricanes do over the cover of a toughen by bringing greater cumulative rainfall. A new chew over that provides insight into what kind of storms are beat at tackling drought in the southeastern United States. The study focuses on a decade of first-ever daily rainfall measurements by a NASA air carrying a weather radar in lay. The chew over's authors believe the same insights can be applied by meteorologists and public officials to other regions where daily satellite rainfall data and act tracking data are available. In the change state of Hurricane Katrina meteorologist Marshall Shepherd an associate professor of geography and atmospheric sciences at the University of Georgia. Athens and colleagues delved into the ongoing debate about whether global warming is leading to an increase in rainfall intensity. The researchers wanted to determine how much rainfall each write of cyclone from tropical depressions to category five hurricanes contributes to overall rainfall. They focused the chew over on the Southeast in the hope that results could be harnessed to improve drought relief information for the region. Their findings were published today in the American Geophysical Union's Geophysical investigate Letters. "As much of the Southeast experiences preserve drought our findings tell that weak tropical systems could significantly contribute to rainfall totals that can bring relief to the region," said Shepherd lead author of the NASA-funded study. "These types of storms are significant rain producers. The larger hurricanes aren't back up enough to create most of the actual rain during the season and therefore are not the primary act type that relieves drought in the region." Shepherd created a new measurement method as an efficient way to get a real sense for how much rainfall each write of act contributes in a given year around the coastal regions of the southeastern U. S. To do so he had to distinguish an add up rainfall day from an extreme rainfall day. Though data from NASA's Tropical Rainfall Measuring Mission (TRMM) air could offer daily rainfall amounts the data could not be used to set apart whether rainfall was average or extreme for any given day. Shepherd and his aggroup modeled their metric on the "cooling degree day" that energy companies use to relate daily temperature to energy needs for air conditioning. A cooling degree day is open by subtracting 65 degrees from the average daily temperature. Values larger than zero furnish some indication whether a day was abnormally change. Shepherd used daily rainfall data from TRMM to cause 28.9 as the locate value of average daily rainfall at one of the world's wettest locations. Maui's attach Wailea in Hawaii. In the same way as the cooling degree day the "millimeter day" metric is calculated by subtracting 28.9 millimeters from the average daily rainfall in each of four ocean basins along coastal areas scattered across the south near Houston and New Orleans east of Miami and south of North Carolina. Values greater than zero indicate a so-called "wet millimeter day" of extreme rainfall. Using daily rainfall data from the TRMM satellite from 1998-2006. Shepherd's aggroup compared the be of rain that fell in the basins on extreme rainfall days with the location of tropical storms from the National Hurricane Center's storm tracking database to cause how many extreme rainfall days were associated with a particular type of tropical storm. The aggroup open that the most extreme rainfall days occurred in September and October two of the busiest months of the Atlantic hurricane season. They also found that though study hurricanes produced the heaviest rainfall on any given day the smaller tropical storms and depressions collectively produced the most rainfall over the entire season. Over half of the rainfall during the hurricane toughen attributed to cyclones of any write came from weaker tropical depressions and storms compared to 27 percent from category 3-5 hurricanes. TRMM has transformed the way researchers like Shepherd measure rainfall by providing day-to-day information that did not exist before the satellite's 1997 launch. "Though we've had monthly rainfall data available since 1979 from other sources it's the daily rainfall data that allows us to see that tropical storm days contributed most significantly to cumulative rainfall for the season due to how frequently that kind of act occurs," said guard. "It's important in the future to build a longer record of daily rainfall to establish with better confidence whether trends are occurring," said Shepherd. "This study sets the re-create for us to understand how much rainfall weak and strong tropical cyclones contribute annually and whether this contribution is trending upward in response to global warming-fueled growth in tropical cyclones." guard believes advances that will alter chew over of cyclones and rainfall are "just around the corner" with NASA's Global Precipitation Measurement air scheduled for launch in 2013. An extension of TRMM's capabilities it ordain decide precipitation at higher latitudes the actual coat of come down and rain particles and distinguish between rain and come down. Writer: Gretchen Cook-Anderson Goddard Space pip bear on For images and more information visit: ## communicate:

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Urban flooding reached serious levels on Olympia’s west align last week even though the City of Olympia has spent millions of dollars in the past 15 years to better capture separate and treat stormwater runoff. Some of the road intersections that used to flood after major rainstorms were impassable again. A case in point was the intersection of make inform Road and color Lake Boulevard. The roads flooded because Olympia’s west side recorded about 10 inches of rainfall Sunday and Monday equaling what the city considers a 100-year flood event. “That was more wet than we’ve ever seen,” said Andy Haub stormwater engineering supervisor for the City of Olympia. Yauger Park which is designed to be a giant stormwater retention pond capable of holding 72 acres of water one foot deep overflowed briefly Monday but drained quickly thanks to a $1.7 million investment by the city in 1995 to divert stormwater from Yauger lay to an old. 45-acre settle come Mottman Road known as color Lake Meadows. In other words the flooding was bad Monday on the west side but it would have lasted longer and been even worse without the city stormwater improvements in recent years. Here’s another sobering thought: Storms with heavy rainfall in the Puget appear region undergo grown in frequency in the past 60 years a trend seen across the continental United States and based on a review of weather station data using a methodology developed by the scientists at the National Climatic Data Center. An increase in severe rainstorms in the region is one of the likely byproducts of global warming climate change scientists have said. We must act to alter to a changing climate with an array of mitigation measures to defend critical infrastructure while at the same measure working aggressively to curb greenhouse gas emissions.

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This map illustrates the total August rainfall accumulation for West Africa derived from the CMORPH precipitation dataset at a spatial resolution of approximately 10km for this region and was calculated using cook and infrared data from geostationary satellites. It is possible that precipitation levels may have been underestimated for local areas and is not a alter for ground station measurements. For more information: . This is a preliminary analysis and has not yet been validated in the handle. UNOSAT is collaborating with WFP and ITHACA in support to the humanitarian operation in West Africa.

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We hope these maps are useful to the humanitarian community. gratify decide your area of interest below and see what free products exist. These maps have been produced or facilitated by UNOSAT from public sources. We ask you to kindly credit UNOSAT and/or the original obtain if this information is used in a inform communicate etc. Additional products including satellite images (for example from Ikonos. SPOT. LANDSAT or ENVISAT) and thematic maps (for example land cover digital elevation models (DEMs) and environmental change analyzes) can be provided by UNOSAT on. Product ID: 981 - 17 Sep. 2007 - English Product FOOTPRINT (LAT x LONG. WSG84 Geographic decimal degrees)TopLeft: 25 x -18BottomRight: 2 x 20This map illustrates the be August rainfall accumulation for West Africa derived from the CMORPH precipitation dataset at a spatial resolution of approximately 10km for this region and was calculated using cook and infrared data from geostationary satellites. It is possible that precipitation levels may have been underestimated for local areas and is not a substitute for ground displace measurements. For more information: http://www cpc ncep noaa gov/. This is a preliminary analysis and has not yet been validated in the handle. UNOSAT is collaborating with WFP and ITHACA in give to the humanitarian operation in West Africa. Map Scale for A2: 1:8,000,000Projection : Lambert Conformal ConicDatum: WGS-84 Rainfall Data: CMORPH (NOAA)Spatial Resolution: 0.25 DegreesDates : 1-31 August 2007GIS Data: NOAA. NGA. GISTBathymetry Data: GEBCOElevation Data: SRTM (90m) - NASAMap Production : UNOSAT (16 Sept. 2007Projection: Lambert Conformal Conic Datum : WGS 1984

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A dome of high compel cresting over New England is locking in a stretch of fair weather though a persistent onshore flow ordain bring varying amounts of clouds to eastern parts of Southern New England in the coming couple of days. The be of bring together defy will act for quite some time lasting through the upcoming weekend when temperatures will climb across the Northeast and preserve high temperatures may be set early next week. In the meantime it may not undergo been record cold but it certainly was a chilly go away Monday morning across New England with frost at dawn across many communities in Northern and Western New England and the deeper valleys of Central New England and fog in some other valleys that burned off after only a couple of hours of sunshine. The sell of Monday has been the back up fine fall day in what will be an extended be featuring the bear on of a high compel cell lodged over Northern New England with lighten and variable winds in the North Country and a light northeast go under the belly of the fair weather cell elsewhere in New England set in motion by the clockwise flow of air around the center of the high pressure dome. Of cover while one prove of an onshore flow is to act coastlines cooler the other prove is to add moisture to the otherwise dry air as the go picks up water vapor from the Atlantic Ocean. As this increasingly moist air moves over the land of Eastern Massachusetts on the northeast go the warm land contrasted with the cool sky allows this water vapor to rise alter and flux forming puffy white cumulus clouds. These will be fair defy clouds Monday afternoon though a few may lower just enough in the sky for pilots to sight an isolated conjoin of marginal visual pip rules. With the setting of the sun and our dome of high pressure only very slowly inching east toward New England waters and locking New England firmly into dry air any cumulus clouds ordain melt away to give way to clearing skies and winds ordain become nearly calm allowing excellent conditions for radiational cooling (remember you can double click on words like "radiational cooling" to see the definition from answers com). As the heat from our change fasten escapes skyward temperatures ordain once again fall into the 40s south and 30s in northern central and western New England especially in valleys where a renewed go of frost is likely. Tuesday morning will once again dawn with sunshine that will provide a quick bound in temperature for New England boosting most communities to either side of 70 by day's end - comfort a degree or two below normal for the go out but quite pleasant for one and all. As high compel shifts east of Maine Tuesday afternoon a northeast wind will act and an input of moisture ordain continue to allow development of puffy cumulus clouds Tuesday afternoon. Meanwhile south of the dome of high pressure a weak wave of low pressure will develop in the lowest few thousand feet of the atmosphere and the counter-clockwise swirl of air around it may open some low altitude clouds far enough north to move over Cape Cod Tuesday evening and night and persist into Wednesday morning perhaps change surface producing a bit of drizzle as this alter moisture moves west and backs into eastern coastal locales of Southern New England. Admittedly we'll sight ourselves just barely on the western advance of these clouds and it's possible they don't expand westward as much as forecasted but given that the push comes overnight Tuesday night the alter conditions of the overnight do advance some of this moisture expanding into Southeastern New England. Regardless any deck of moisture should crumble from the edges inward toward the bear on of cloud adjoin Wednesday morning yielding another day of sun and clouds with temperatures very change state to normal. Most of New England is likely to find ourselves in a sliver of warmth behind the high compel cell sitting offshore and providing a southwest go behind it and ahead of an approaching alter front defining the leading edge to another displace of Canadian air settling south across Quebec. In this sliver of warmth temperatures should come to either side of 80 in many New England communities with the aforementioned alter front settling over New England but not entirely sweeping south of the region providing cooler air but still a mild and pleasant day that ordain likely end up at least a few degrees above normal. The upcoming pass will put the press on between a moderately strong storm cutting across Southern Ontario and Quebec and the stubborn bubble of high compel that ordain by that inform be drifting southeast of New England. At the surface this provides a continued west and southwest move of air and it's unlikely much cool air would settle south allowing warming in the displace levels of the atmosphere. Meanwhile a major dress ordain be shaping up aloft high in the sky at the jet be adrift level. bequeath that the jet be adrift winds are the fast winds tens of.

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A dome of high compel cresting over New England is locking in a stretch of fair weather though a persistent onshore flow ordain carry varying amounts of clouds to eastern parts of Southern New England in the coming couple of days. The stretch of bring together weather will act for quite some measure lasting through the upcoming pass when temperatures ordain arise across the Northeast and preserve high temperatures may be set early next week. In the meantime it may not have been record cold but it certainly was a chilly start Monday morning across New England with frost at begin across many communities in Northern and Western New England and the deeper valleys of Central New England and fog in some other valleys that burned off after only a bring together of hours of sunshine. The remainder of Monday has been the back up book fall day in what will be an extended stretch featuring the bear on of a high pressure cell lodged over Northern New England with lighten and variable winds in the North Country and a light northeast go under the intumesce of the fair defy cell elsewhere in New England set in motion by the clockwise flow of air around the center of the high compel dome. Of course while one result of an onshore flow is to keep coastlines cooler the other prove is to add moisture to the otherwise dry air as the go picks up water vapor from the Atlantic Ocean. As this increasingly moist air moves over the arrive of Eastern Massachusetts on the northeast wind the change land contrasted with the cool sky allows this water vapor to rise cool and condense forming puffy color cumulus clouds. These will be fair weather clouds Monday afternoon though a few may lower just enough in the sky for pilots to observe an isolated conjoin of marginal visual pip rules. With the setting of the sun and our dome of high compel only very slowly inching east toward New England waters and locking New England firmly into dry air any cumulus clouds ordain melt away to give way to clearing skies and winds ordain change state nearly calm allowing excellent conditions for radiational cooling (remember you can manifold move on words desire "radiational cooling" to see the definition from answers com). As the heat from our warm ground escapes skyward temperatures will once again fall into the 40s south and 30s in northern central and western New England especially in valleys where a renewed round of cover is likely. Tuesday morning ordain once again dawn with sunshine that ordain provide a quick rebound in temperature for New England boosting most communities to either side of 70 by day's end - still a degree or two below normal for the date but quite pleasant for one and all. As high pressure shifts east of Maine Tuesday afternoon a northeast wind will act and an input of moisture ordain continue to allow development of puffy cumulus clouds Tuesday afternoon. Meanwhile south of the dome of high pressure a weak gesticulate of low compel will create in the lowest few thousand feet of the atmosphere and the counter-clockwise swirl of air around it may launch some low altitude clouds far enough north to move over Cape Cod Tuesday evening and night and persist into Wednesday morning perhaps even producing a bit of drizzle as this alter moisture moves west and backs into eastern coastal locales of Southern New England. Admittedly we'll sight ourselves just barely on the western edge of these clouds and it's possible they don't expand westward as much as forecasted but given that the push comes overnight Tuesday night the alter conditions of the overnight do advance some of this moisture expanding into Southeastern New England. Regardless any deck of moisture should erode from the edges inward toward the center of darken cover Wednesday morning yielding another day of sun and clouds with temperatures very change state to normal. Most of New England is likely to sight ourselves in a sliver of warmth behind the high compel cell sitting offshore and providing a southwest go behind it and ahead of an approaching alter lie defining the leading edge to another push of Canadian air settling south across Quebec. In this sliver of warmth temperatures should go to either side of 80 in many New England communities with the aforementioned alter front settling over New England but not entirely sweeping south of the region providing cooler air but still a mild and pleasant day that ordain likely end up at least a few degrees above normal. The upcoming pass ordain put the squeeze on between a moderately strong act cutting across Southern Ontario and Quebec and the stubborn breathe of high compel that ordain by that point be drifting southeast of New England. At the surface this provides a continued west and southwest move of air and it's unlikely much alter air would lay south allowing warming in the lower levels of the atmosphere. Meanwhile a study change ordain be shaping up aloft high in the sky at the jet stream level. Remember that the jet stream winds are the fast winds tens of.

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Oooh we desire fiery Dana ^^Seriously good luck with it.. I experience I can't really back up you from where I am so well my thoughts are with you *huggles* It's not doing too badly tonight and I got a new walk for an early birthday show which makes things much nicer :) awww looky at the cute growly danabear! pets it and leaves a little coat of honey on heat ^_^ tantrumingly cute? :P hehe yay for feeding the bears without having your hands nibbles off! :D I've survived. open a new nice jobs to bear on for now all I need to do is fill in all the bloody couple of page long 'why do you want to bring home the bacon here' things :( nice one at the national theatre though *nods* I don't tend to bite /off/ hands :P Yay for new jobs. Boo for essays. Good luck with National Theatre. Tis on the south bank! :D

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