Alton is a village and civil parish in Staffordshire, England. In 2001 there were 1,243 people living in Alton. There is Alton Towers nearby.
Godalming
Godalming is a town and civil parish in Surrey, England. In 2011, there were 21,804 people living in Godalming.
Godalming has a railway station, Godalming railway station. The station is on the Portsmouth Direct Line, which goes between Portsmouth and London Waterloo. This line is served by South Western Railway.
Roads that go through or near Godalming are:
Godalming is around 31 miles or 50 kilometres away from Gatwick and Heathrow Airport.
Retford
Retford is a town near the A1 road in Nottinghamshire, England.
Maltby
Maltby is a town and civil parish in South Yorkshire, England. In 2001 there were 17,247 people living in Maltby.
Mansfield
Mansfield is a town in Nottinghamshire, England. There is also the smaller settlement of Mansfield Woodhouse to the north. The town is surrounded by a pocket of steep hills within the Maun Valley. It has a population of about 67,885.
North Walsham
North Walsham is a town in North Norfolk, England. In 2001 there were 11,998 people living in North Walsham.
Dereham
Dereham is a town and civil parish in Breckland District, Norfolk, England. In 2001 there were 15,659 people living in Dereham.
Grantham
Grantham is a town near the A1 road in Lincolnshire, England. Margaret Thatcher was born here, and Isaac Newton went to school here. Grantham is famous for its gingerbread.
The town is a relatively small town but has multiple satellite villages. It has numerous estates, such as Gonerby Hill Foot, Manthorpe, Earlesfield and Alma Park.
There are several schools in the town, such as the Priory Ruskin Academy and the Kings Grammar School, which Isaac Newton attended.
Colsterworth
Colsterworth is a village and civil parish in Lincolnshire, England. The parish contains the hamlet of Woolsthorpe-by-Colsterworth. In 2001 there were 1,508 people living in Colsterworth.
Dacre
Dacre is a village and civil parish in Eden, Cumbria, England. In 2001 there were 1,326 people living in Dacre.
Dacre, North Yorkshire
Dacre is a village and civil parish in North Yorkshire, England. In 2001 there were 658 people living in Dacre.
Culgaith
Culgaith is a village and civil parish in Eden, Cumbria, England. In 2001 there were 721 people living in Culgaith.
Tebay
Tebay is a village and civil parish near the M6 motorway in Cumbria, England. In 2001 there were 728 people living in Tebay.
Crosby Ravensworth
Crosby Ravensworth is a village and civil parish in Eden, Cumbria, England. In 2001 there were 538 people living in Crosby Ravensworth.
St Austell
St Austell is a town on the A390 road, in Cornwall, England. It is near an area of granite moorland where large quantities of china clay are produced. The district is full of disused clay pits and large mounds of waste material. The Eden Project has been built on the site of former china clay workings. St Austell's population is the largest of any town or city in Cornwall.
Shap
Shap is a village and civil parish in Eden, Cumbria, England. In 2001 there were 1,221 people living in Shap.
Dufton
Dufton is a village and civil parish in Eden, Cumbria, England. In 2001 there were 169 people living in Dufton.
Broxted
Broxted is a village and civil parish in Uttlesford, Essex, England. In 2001 there were 526 people living in Broxted.
Chickney
Chickney is a village and civil parish in Uttlesford, Essex, England. In 2001 there were 38 people living in Chickney. Chickney has a church called St Mary's Church, Chickney.
Rainband
A rainband is an area of rainfall where all the clouds and precipitation are stretched out in a long line or band. Rainbands can be stratiform or convective. They are caused by differences in temperature. When seen on a weather radar, the long narrow shape is called a banded structure. Rainbands in a tropical cyclone are curved and may even spiral around the center of the cyclone. Tropical cyclone rainbands include rain showers and thunderstorms. When this includes an eyewall and the eye, they make a hurricane or tropical storm. The size of rainbands around a tropical cyclone helps to measure the cyclone's intensity.
Rainbands that form near and ahead of cold fronts can be squall lines which can produce tornadoes. The shape of rainbands linked with cold fronts can be changed by mountains. The mountains block the winds which can then form a low-level barrier jet. Bands of thunderstorms can form when sea breeze and land breezes meet, if enough moisture is present. Sometimes sea breeze rainbands which are ahead of a cold front, can hide the location of the cold front itself. Rainbands in an extratropical cyclone can cause large amounts of rain or snow. Behind extratropical cyclones, rainbands can form downwind of large, warmer bodies of water such as the Great Lakes. If the air is cold enough, these rainbands can cause heavy snowfalls.
Rainbands ahead of warm occluded fronts and warm fronts have little upward motion. They tend to be wide and stratiform in nature. In an atmosphere with rich low level moisture and vertical wind shear, narrow, convective rainbands form. These are known as squall lines, and are usually in the cyclone's warm sector, ahead of strong cold fronts associated with extratropical cyclones. Wider rain bands can form behind cold fronts, which usually have more stratiform, and less convective, precipitation. In colder cyclones, small bands of heavy snow can occur with a width of to . These bands are linked with areas of frontogensis, or zones of strengthening temperature contrast. The curved air flow from extratropical cyclones bringing cold air across the relatively warm Great Lakes can lead to narrow lake effect snow bands. These can bring heavy localized snowfalls.
Rainbands exist on the edges of tropical cyclones, and point towards the cyclone's center of low pressure. Rainbands within tropical cyclones need moisture and a low level pool of cooler air. Bands located to from a cyclone's center move outward. They can cause heavy rains and squalls of wind, as well as tornadoes. Some rainbands move closer to the center, forming a secondary, or outer, eyewall within intense hurricanes. Spiral rainbands are such a basic part of a tropical cyclone that in most tropical cyclone basins, use of the satellite-based Dvorak technique is the main method used to determine a tropical cyclone's maximum sustained winds. Using this method, the area of spiral banding and difference in temperature between the eye and eyewall is used to estimate the maximum sustained wind and a central pressure.
Convective rainbands can form parallel mountains on their windward side. This is due to lee waves triggered by hills just upstream of the cloud's formation. Their spacing is normally to apart. When rainbands near frontal zones get close to steep mountains, a low-level barrier jet stream forms parallel to and just before the mountain ridge. This slows down the frontal rainband just before the mountain barrier. If enough moisture is present, sea breeze and land breeze fronts can form convective rainbands. Sea breeze front thunderstorm lines can become strong enough to hide the location of an approaching cold front by evening. The edge of ocean currents can cause thunderstorm bands due to heat differences where they meet. Downwind of islands, rainbands can form when low level winds meet downwind of the island edges. Offshore California, this has been noted in the wake of cold fronts.
ÖFB-Frauenliga
The ÖFB-Frauenliga (German for ÖFB Women's League) is the highest level of Women soccer in Austria. The most successful team was USC Landhaus Wien with 12 titels, in the last years SV Neulengbach was the best club in Austria winning all titels from 2003/04 on.