With an outstanding view in which to enjoy your dining experience, there is a lot to like about this restaurant. Fog daily 17th - 21st December (London/South).
Both December 1819 & January 1820 were notably cold (though not in the 'top-10' of such-named months), and the overall winter season figure of 1.4degC represented an anomaly of around -2.3C on the all-series mean and was ranked just outside the top-20 of coldest winters by this measure. ](See Burt & others, 'Weather'/RMetS/August 2005).
. Stone bridges and houses washed away in 5 or 6 counties, coastline altered at river mouths.
Night Temperature 9.8 °C 50 °F.
In 1841, the census total for Ireland was 8.17mn; by the 1851 tally, it had fallen to 6.55mn: it has been estimated that over 1mn people died due to the Famine. At the end of they year, John Oram says . At Torquay and Sidmouth, Devon over 30 cm of snow fell.
Dover and Deal in Kent and Brighton, East Sussex, became completely cut off. There was severe flooding on tributaries of the River Aire & reservoir failure at Adel, Leeds (W. Yorkshire) in this month. Almost continuous frost 23rd to 31st December 1829, 12th to 19th January 1830 and then 31st January to 6th February. April to August ... notably and persistently cold by CET series. One of the best spots in Cornwall for the whole family is the Camel Creek Adventure Park located in Wadebridge. Be sure to watch your head on the low ceiling while enjoying a wonderfully cozy atmosphere. Thick fog 22nd to 25th February (London/South).
Camel Creek Adventure Park. One of the driest years across England and Wales using the EWP series. Part of a notably dry period in the mid/late 1850s: see below. a cold backward spring up 'till May which month was remarkably dry .
In the Greenwich record, the total rainfall for the three months of June, July & August=285mm (188%), with June exceptionally wet at 277% of LTA for that station.
(Easton, in CHMW/Lamb). . The May and June of 1815 were very unsettled, and marked by high rainfall totals across the Low Countries. Over the period 17th/18th November, 1893, as a vigorous depression moved from SW Scotland to the southern North Sea, high winds caused considerable damage across northern areas of Ireland, much of Scotland (even normally sheltered spots), near the west & north coast of Wales & more irregularly inland elsewhere.
In particular, the heavy rain-storms in the lead up to, and immediately prior to the Battle of Waterloo (17th/18th) across Belgium may have been a contributory factor in the defeat of the Napoleonic French forces - the French cavalry in particular finding it difficult to traverse the rain-sodden ground. Many trees were blown down across Ireland, the English Midlands & in counties bordering the English south coast. A notably wet summer (157% of LTA 1916-1950) across England & Wales (see Lamb/CHMW).