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bulging upper parts. These clouds resemble very small ragged cumulus and are often accompanied by fibrous trails of virga from their bases. Altocumulus floccus with virga, base 15,000 ft London Heathrow Airport Altocumulus castellanus, base 7,000 ft Great Gaddeston, Herts Altocumulus castellanus

on the Isles of Scilly in autumn 2054 and 131mm/h over an isolated grid box in the Outer Hebrides in summer 2030. Due to their localised nature, both these events appear unphysical. However, 136mm/h simulated over London in summer 2070 appears plausible as it occurs alongside other very intense

A (2003) Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J Geophys Res 108(D14):4407. doi:10.10 29/2002JD002670 Riehl H (1979) Climate and weather in the tropics. Academic Press, London, p 595 Rossow WB, Schiffer RA (1991

increases from 5 to 24 through adding TTA to the 3-site network). The two GAUGE stations, on an annual time-frame, do not significantly alter the English emission estimates but do give greater clarity to London and the North East. They would also allow smaller (sub-annual) time windows

five warmest springs in a temperature series that extends back to 1910. The standout spring statistic, however, is found within the Central England Temperature (CET) series. A record of temperatures covering a roughly triangular section of England from Lancashire in the north to London in the east

name Orkney and Shetland Highland and Eilean Siar Grampian Tayside Strathclyde Dumfries, Galloway, Lothian Northern Ireland Yorkshire and the Humber Northeast England East Midlands East of England London and Southeast England Northwest England West Midlands Southwest England Wales uk United Kingdom

, Canada and UK Aid, London, United Kingdom. Available online at: www.idrc.ca/cariaa Hegger, D., & Dieperink, C. (2014). Toward successful joint knowledge production for climate change adaptation: lessons from six regional projects in the Netherlands. Ecology and Society, 19(2). http://doi.org/10.5751/ES

. at river catchment or on urban scales. Instantaneous screen level temperature (degrees Kelvin) in a 100 m simulation over London. The detailed signature of small-scale features in the land surface (e.g. valleys and the River Thames) are visible. 24 25 Future observations to support high resolution model

JULY 2014 W A N G E T A L . 5265 TABLE 1. Twelve selected weather stations (UA denotes an upper air reporting station). No. Weather station Longitude Latitude Abbreviation 001 Windsor Airport 82896 0 W 42828 0 N WDA 002 London Int’l Airport 81815 0 W 43803 0 N LIA 003 Toronto Lester B. Pearson

predictions provided by such models could be used for both realtime forecasting of weather hazards and for long term planning purposes, for example to help inform local air quality policy and regulation. Figure 16 - Instantaneous screen level temperature (degrees Kelvin) in a 100m simulation over London