DOCSLIB.ORG

Southern Uplands

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Southern Uplands MOUNTAIN WEATHER INFORMATION SERVICE www.mwis.org.uk Southern Uplands The Galloway hills eastward to the Lammermuir hills. The Cheviots (including higher hills within the adjacent Northumberland NP). Would you like to sponsor this forecast and reach the thousands of walkers and climbers that use MWIS every day? Contact us for details on promoting your business now! General Summary for Sunday, 18 April, 2021 British Mountain Summary: Based on forecast chart for noon 18 April, 2021 Windy with rain on and off near the west coast of Scotland north of Mull. A little rain elsewhere in Scotland, mainly morning. Dry in England and Wales, most summits clear of cloud and little wind at all. Headline for Southern Uplands A little rain and fog for western hills; mainly Galloway. Detailed Forecast for Sunday, 18 April, 2021 How windy? (On the Southerly, 15mph The Cheviot and near the Lothians to 20, perhaps 25mph in morning summits) Galloway. Effect of wind on Fairly small. you? How wet? Patchy rain western hills, mainly morning. Little if any further east (Precipitation and its Light rain now and again morning almost all west of M74; will fizzle out almost impact) completely into the afternoon. A little light rain may reach the Pentland hills. Cloud on the hills? Most summits cloud free; may form at times Galloway. Galloway: Hills intermittently cloud free, but banks of cloud for periods above 600m, occasionally 350m near the coast. Elsewhere: summits cloud free. Chance of cloud Almost certain, although 40% Galloway free summits? Sunshine? Ranging from cloudy western hills to intermittent sunshine Borders, although this may Air clarity (below be through high thin cloud. cloud) Very good or excellent visibility. How Cold? (at 750m) 4C Freezing Level Above the summits. Frost widely at dawn in valleys and upland areas sheltered from the wind. Visit us at www.mwis.org.uk Page 1 of 2 Live SU 2021-04-18 2021-04-20 MOUNTAIN WEATHER INFORMATION SERVICE www.mwis.org.uk Southern Uplands - Looking Ahead Monday 19 April Tuesday 20 April How windy? (On the Southerly, 15mph. although 10mph near Low confidence in this forecast. summits) Lothians and Cheviot hills. Direction may well vary, less than 15mph. Effect of wind on Mostly negligible. Small you? How wet? Rain not expected Bursts of rain (Precipitation and its Frequently dry, although increasingly threat impact) of an hour or two of steady rain, or perhaps heavier but briefer showers. Cloud on the hills? Confined to western hills Extensive on higher areas Near and west go M74: Extensive above The mountains extensively foggy above 500 600m and at lower near the coast. to 700m, although patches may form on Elsewhere: summits cloud free. lower slopes near the Solway. Chance of cloud 60% 50% free summits? Sunshine? Patchwork of sunshine. Little sunshine; frequently very god visibility. Air clarity (below Slight haze. cloud) How Cold? (at 3 to 5C; coldest Galloway 4C 750m) Freezing Level Above the summits. Above the summits. Planning Outlook All mountain areas of Britain from Monday, 19 April, 2021 Rain will erratically transfer to eastern Scotland and may break out in England and Wales on Tuesday - although the timing is uncertain. Then as pressure then builds again, fine weather will return. Although the wind will temporarily revert to northerly, the air drawn in will be less cold than recently. There may still be valley frost at night but daytime temperatures will be higher and freezing level only temporarily near 900m on Tuesday and Wednesday in Scotland. Widely very dry underfoot; beware fire risk. Forecast issued at 7:47 on Sunday, 18 April, 2021 The production of the Scottish forecasts is fully funded by the Scottish Government through Mountaineering Scotland with the support of sportscotland. Forecasts are issued daily by 16:30 and are kept under review and amended as necessary. However, expected conditions can still change after issue. © Copyright Mountain Weather Information Service, 2021. Visit us at www.mwis.org.uk Page 2 of 2 Live SU 2021-04-18 2021-04-20.
Load more

Recommended publications
  • TA 7.3 SNH Baseline Landscape Character
    EUCHANHEAD RENEWABLE ENERGY DEVELOPMENT Technical Appendix 7.3: SNH Baseline Landscape Character 10/2020 www.stephenson-halliday.com A. Technical Appendix 7.3: Baseline Landscape Caracter A.1 SNH Landscape Character Assessment (2019) A.1.1 SNH recently republished their National Programme of Landscape Character Assessments as a digital map based LCA in 2019. This data was reviewed to take account of intervening technical improvements in website mapping to produce a revised national suite of landscape character type at 1:50,000 scale. This information was created in collaboration and consultation with FLS and HES as well as all local authorities. This also included a more consistent baseline description across Scotland. As this is an online document, the following is an extract of the landscape character citations for each character area assessed. A.1.2 Compiled within this document are the following SNH Landscape Chatacter Type Baseline documents: • LCT 073 - Upland Glen - Ayrshire (2019) • LCT 081 - Southern Uplands - Ayrshire (2019) • LCT 160 - Narrow Wooded Valley - Dumfries & Galloway (2019) • LCT 165 - Upper Dale - Dumfries & Galloway (2019) • LCT 166 - Upland Glens - Dumfries & Galloway (2019) • LCT 175 - Foothills - Dumfries & Galloway (2019) • LCT 177 - Southern Uplands - Dumfries & Galloway (2019) • LCT 178 - Southern Uplands with Forest - Dumfries and Galloway (2019) Technical Appendix 7.3: Baseline Landscape Caracter 1 SNH National Landscape Character Assessment Landscape Character Type 73 UPLAND GLEN - AYRSHIRE Location and Context The Upland Glen- Ayrshire Landscape Character Type occurs in three places in Ayrshire, focused to the far south and east; the valley of the Afton Water, immediately to the south of New Cumnock, and Glen Tig and Glen App, draining to the Ayrshire coast, close to the boundary with Dumfries and Galloway.
    [Show full text]
  • Regional Scenic Areas Technical Paper;
    DUMFRIES AND GALLOWAY COUNCIL Local Development \ Plan Technical Paper Regional Scenic SEPTEMBER 2014 Areas www.dumgal.gov.uk Dumfries and Galloway Regional Scenic Areas Technical Paper; Errata: Regional Scenic Areas were drawn as part of the 1999 Dumfries and Galloway Structure Plan. The adopted boundaries were shown on plans within Technical Paper 6 (1999) and subsequently in the four Local Plans, adopted in 2006. The boundaries were not amended during the production of the 2014 RSA Technical Paper; however the mapping included several errors: 1. Galloway Hills RSA The boundary to the east of Cairnsmore of Fleet (NX 501670) should have included Craigronald and Craigherron but not High Craigeazle, Low Craigeazle or Little Cullendoch Moss (Maps on pages 12 and 19 should be revised as below): Area not in RSA Area should be in RSA Area not in RSA 2. Solway Coast RSA (two areas); St Mary’s Isle, Kirkcudbright (NX 673491) should have been included within the RSA boundary (Maps on pages 12 and 24 should be revised as below): Area should be in RSA The area to the west of Powfoot (NY 148657) should have been included within the RSA (Maps on pages 12 and 24 should be revised as below): Area not within RSA Area should be in RSA 3. Terregles Ridge RSA The area around the A711 at Beeswing (NX 897694) should not have been included within the RSA (Maps on pages 12 and 27 should be revised as below): Area not within RSA Technical Paper: Regional Scenic Areas Contents Page Part 1: Introduction 2 Regional Scenic Designations 2 Dumfries and Galloway Landscape Assessment 3 Relationship between the Landscape Assessment and Scenic Designations 3 Part 2: 1999 Review Process 5 Aims and Objectives 5 Methodology 5 Part 3: Regional Scenic Area Descriptions 8 Appendices 42 Appendix 1: References 42 Appendix 2: Landscape Character Types and Units 43 1 Part 1: INTRODUCTION The quality of the landscape is one of Dumfries and Galloway's major assets, providing an attractive environment for both residents and visitors.
    [Show full text]
  • R01 HSUK Scottish Rail Strategy
    HSUK SCOTTISH RAIL STRATEGY With Edinburgh and Glasgow comprising two of the UK’s principal conurbations, it is natural that both cities will be primary stakeholders in any future UK high speed rail network. Projections for HS2 show high speed lines extending northwards to both Edinburgh and Glasgow, and the scheme’s proponents claim major economic benefits accruing from accelerated North-South links, and environmental benefits accruing from short-haul air flows converted to rail. It is important to appreciate that the core rationale of any high speed rail system is to connect primary conurbations (of 500,000+ population), and this is likely to deter the opening of new lines north of the Forth-Clyde Line. Hence a major proportion of the Scottish population away from the Central Belt seems likely to see no direct benefits from the UK high speed rail project. These areas have been poorly served by rail since the ‘Beeching’ cuts of the 1960’s, and the economic impacts are continuing. The Scottish Government has taken significant steps to redress these connectivity deficiencies, with several rail routes reopened in recent years. But whilst the pace of Scottish reopenings far outstrips performance elsewhere in the UK, progress is still slow. It seems vital that the UK high speed rail initiative is developed in such a way as to extend operation of high speed services north of the Forth-Clyde Line, and in doing so to spur further reopenings. This will bring benefit to the widest practicable spread of Scottish communities. The following diagrams chart the development of the Scottish rail network, and illustrate the likely impacts of both HS2 and the alternative High Speed UK scheme.
    [Show full text]
  • Front Matter
    Scottish Journal ISSN: 0036 9276 of GEOLOGY / Volume 35, Part 2, pages 97-192 1999 Published by the Geological Society Publishing House for the Geological Societies of Edinburgh and Glasgow The Scottish Journal of Geology continues the Transactions of the Edinburgh Geological Society and the Transactions of the Geological Society of Glasgow, and is sponsored by the councils of the two societies. It contains two parts per volume. The Journal is sent to members of both societies. Details of membership may be obtained from the secretaries, whose names appear below. Contributions or legacies to assist towards the cost of publication of the Journal would be welcomed by the Editorial Board. EDITORS COLIN BRAITHWAITE ROB DUCK PHIL STONE ROBERT CHEENEY PETER HILL ROY THOMPSON TIM DEMPSTER SUE RIGBY PUBLISHING HOUSE STAFF EDITOR HELEN KNAPP (e-mail: [email protected]) Secretaries of Societies EDINBURGH GLASGOW J. MICHAEL DEAN DR I. ALLISON 6 Corrennie Gardens Faculty of Science Edinburgh University of Glasgow EH10 6DG Glasgow, G12 8QQ Front cover illustration Load casts on the base of a greywacke turbidite bed from until the latter part of this century and some aspects are still the Upper Ordovician Kirkcolm Formation of the Southern valid. It is only relatively recently that application of sedi- Uplands. This example is exposed on the west coast of the mentology, linked with models arising from the plate tectonic Rhins of Galloway at Slocknamorrow, near Portobello and revolution, has led to a fundamental re-interpretation of about 13 km NNW of Portpatrick. In areas of complex Southern Uplands structure in terms of subduction and folding and steeply inclined beds it is features such as these terrane accretion.
    [Show full text]
  • A Landscape Fashioned by Geology
    64751 SNH SW Cvr_5mm:cover 14/1/09 10:00 Page 1 Southwest Scotland: A landscape fashioned by geology From south Ayrshire and the Firth of Clyde across Dumfries and Galloway to the Solway Firth and northeastwards into Lanarkshire, a variety of attractive landscapes reflects the contrasts in the underlying rocks. The area’s peaceful, rural tranquillity belies its geological roots, which reveal a 500-million-year history of volcanic eruptions, continents in collision, and immense changes in climate. Vestiges of a long-vanished ocean SOUTHWEST are preserved at Ballantrae and the rolling hills of the Southern Uplands are constructed from the piled-up sediment scraped from an ancient sea floor. Younger rocks show that the Solway shoreline was once tropical, whilst huge sand dunes of an arid desert now underlie Dumfries. Today’s landscape has been created by aeons of uplift, weathering and erosion. Most recently, over the last 2 million years, the scenery of Southwest Scotland was moulded by massive ice sheets which finally melted away about 11,500 years ago. SCOTLAND SOUTHWEST A LANDSCAPE FASHIONED BY GEOLOGY I have a close personal interest in the geology of Southwest Scotland as it gave me my name. It comes of course from the town of Moffat, which is only a contraction of Moor Foot, which nestles near the head of a green valley, surrounded by hills and high moorland. But thank God something so prosaic finds itself in the midst of so SCOTLAND: much geological drama. What this excellent book highlights is that Southwest Scotland is the consequence of an epic collision.
    [Show full text]
  • Regional Geochemical Patterns in South-East Scotland: Source Lithology, Inheritance and Glacial Overprinting
    Published in Scottish Journal of Geology, 2013, Volume 49, 33-40. Note that this version of the text does not include the Journal’s editorial and proof corrections Regional geochemical patterns in south-east Scotland: source lithology, inheritance and glacial overprinting P. Stone and A. A. McMillan British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA [email protected] Synopsis The Lower Palaeozoic, Southern Uplands terrane shows a NE-SW, strike-parallel coincidence of regional geochemical lineaments defined from stream sediment data, and major, lithostratigraphically significant structures. West of Moffat, Silurian strata of the Gala and Hawick groups are divided by geochemical lineaments coincident with the Laurieston Fault. East of Moffat the geochemical lineaments diverge towards the north-east with Gala-type regional geochemistry (high Sr and Ba, low CaO) to the north of the Moffat Valley Fault, whilst Hawick-type regional geochemistry (low Sr and Ba, high CaO) continues to the south of the Laurieston Fault; between the faults lies the recently defined Ettrick Group. Beyond the eastern end of the Lower Palaeozoic outcrop its geochemical lineaments extend across the unconformable cover of Devonian ‘Old Red Sandstone’. This is partly a drainage catchment effect, but two other possible explanations are considered: a localized derivation of the Devonian clastic rocks such that they inherit the compositional patterns of the underlying Lower Palaeozoic sandstones, or a geochemical signature imposed by glacial deposits derived from the Lower Palaeozoic outcrop. The local effect of glacial dispersion is confirmed by the distribution of TiO2; anomalously high levels associated with Carboniferous mafic lavas have been transported north-east across the low-TiO2 Carboniferous sedimentary rocks of the Tweed Basin.
    [Show full text]
  • THE SOUTHERN UPLANDS PARTNERSHIP Galloway Glens Biosphere Experience Project Report
    Galloway Glens Biosphere Experience Final Project Report September 2018 – March 2020 = Company No. 200827 registered in Edinburgh Charity No. SC029475 T:01750 725 154 1 www.sup.org.ukTHE SOUTHERN UPLANDS PARTNERSHIP Galloway Glens Biosphere Experience Project Report Contents Contents ........................................................................................................................................................... 2 Introduction ...................................................................................................................................................... 3 Who Was Involved in the Project? ........................................................................................................... 3 Objectives fit with LEADER Strategy and HLF Outputs........................................................................ 3 Funding ......................................................................................................................................................... 4 Project Experience .......................................................................................................................................... 5 Delivery and Actions ................................................................................................................................... 5 Training and Networking ............................................................................................................................ 5 Events ..........................................................................................................................................................
    [Show full text]
  • The Geography of Scotland Thesis
    THE GEOGRAPHY OF SCOTLAND BY ROBERT ROLAND DRUMMOND B. S., Indiana State Teachers College, 1939 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN GEOGRAPHY IN THE GRADUATE SCHOOL OF THE UNIVERSITY OF ILLINOIS, 1940 URBANA, ILLINOIS UNIVERSITY OF ILLINOIS THE GRADUATE SCHOOL May 25? 1940 I HEREBY RECOMMEND THAT THE THESIS PREPARED UNDER MY SUPERVISION t w Robert Roland Drummond______________________ ENTITLED___________ THE GEOGRAPHY OF SCOTLAND________________ BE ACCEPTED* AS FULFILLING THIS PART OF THE REQUIREMENTS FOR THE DEGREE OF. Master of Science In Geography U i In Charge oFThesis Head of Department Recommendation concurred inf Committee on Final Examinationf ♦Subject to successful final examination in the case of the doctorate. •{•Required for doctor’s degree but not for master’s. 1000— 4-40— 18703-S TABLE OP COBTESTS Chapter Page X. Introduction 1 XX* Historical Background . • • • ............ * . 2 XXX. Geographical Regions of Scotland •«••*»**• 6 A* Introduction • *•••*«•••••»••• 6 B* Ha© South of Scotland *•••*•••*«** 8 1* Physical Features . • # ............ .. * 8 3* ClisM&te ##•***♦♦•♦*••••• IS S. Natural Resources • • ............ .. 1 9 4* Agriculture .............. 22 5. Industries 37 a* Woolen ^Manufacturing •*•*••• 3 7 C* The Midland Valley .............. .. 3 9 1. H i y s l e a l F e a t u r e s * * « • .............. 3 9 2* Climate • ............ .................. .. 4 3 3 * natural Resources ......................................... • 45 a. Coal * . .................. * . * . 4 6 h. Oil Shales ......... .. 6 2 4« Agriculture . • • .............. .. • . 67 5. Industries * • « .............. 7 9 a« Iron and Steel Production • • « . * 79 b. Shipbuilding «.•«••••••• 8 3 c. rjoglneering Industries 38 d» Tesctiles *■******••••*• 8 9 e. Printing and Publishing ......... .. 9 6 f • Other Industries »••«•••*• 9 6 Dm Ifce Highlands *•».•«•••••*•••• 97 1* fftysical Features » • • .............
    [Show full text]
  • Southern Uplands
    2019 The Forests of the Southern Uplands Clinging to the slopes of heather-clad hills and 5 flanking the sides of tumbling streams, the forests 4 2 of the Southern Uplands straddle the natural barrier between England and Scotland. Remains of hill forts and cairns are a reminder of turbulent times in the area, but today, these now peaceful lands offer a wide range of walks in some special places. Explore further... Our waymarked trails follow Keep your eyes open... Beyond our waymarked trails, if you 3 graded paths so you can find fancy heading out on your own, one that’s just right for you. Forests are great places for wildlife. The there are miles of forest tracks and All the trails in this leaflet trees create lots of different habitats, from 6 un-signed paths to discover. have clear signs so you can the airy canopy to the sheltered heather on 1 follow the route even if the forest floor or the insect hotels of rotting you’ve never visited the stumps. Just take the time to sit quietly in any Remember that you are in a forest before. forest and you’ll see and hear something of working forest. Our management the wealth of activity among the trees, from work helps these great forests If you’re into mountain biking, there’s loads flowers and insects to birds and mammals. become even more diverse and to do in this area. Ae, Dalbeattie, Mabie and attractive for wildlife and visitors, Newcastleton are part of the 7stanes: The Forest of Ae and the forests around forestryandland.gov.scot/7stanes Eskdalemuir are recognised nationally for as well as supplying timber for use red squirrel conservation, whilst the upper in our everyday lives.
    [Show full text]
  • Edinburgh Rock—The Geology of Lothian, by Euan Clarkson & Brian Upton, 2006
    Journal of Sedimentary Research An International Journal of SEPM Colin P. North and Kitty L. Milliken, Editors A.J. (Tom) van Loon, Associate Editor for Book Reviews Review accepted 8 August 2006 Edinburgh Rock—The Geology of Lothian, by Euan Clarkson & Brian Upton, 2006. Dunedin Academic Press, Hudson House, 8 Albany Street, Edinburgh, EH1 3QB Great Britain. Hardback, 239 pages. Price GBP 16.95; USD 35.00; EUR 27.00. ISBN 1 903765 39 0. Deep time; think of those really amazing, fundamental changes to the world of geological ideas: continental drift, the theory of evolution, uniformitarianism. The greatest, and most fundamental change was the concept of “deep time,” an Edinburgh idea, a contribution from James Hutton: geological processes are to be measured in millions, rather than a mere few thousand years. Deep time—a resonant term, echoing out of the world of Edinburgh geology for two hundred years. The compass of this book is the area south of the Firth of Forth, defined by the Bathgate Hills in the west, by the northernmost part of the Southern Uplands to the south, and to the east by Siccar Point, south of Dunbar. If geologists were given to going on pilgrimages, surely Siccar Point would be the place to go, the place where Deep Time was revealed. This is a beautiful book; the publishers are to be congratulated, good quality paper, superb print quality, excellent illustrations; the colour and design of the maps is brilliant; Polskabook did a fine job of printing and binding. You hold this book and feel a sense of bibliographical well-being.
    [Show full text]
  • Forest Habitat Networks in the Scottish Borders ______17 7
    Native Woodland Habitat Networks in the Scottish Borders Duncan Ray, Kevin Watts, Matthew Griffiths, Christine Brown and Louise Sing, Forest Research REPORT of a study funded by Forestry Commission Scotland, Scottish Natural Heritage, and Scottish Borders Council in 2003. Native Woodland Habitat Networks in the Scottish Borders _____________________ 1 _______________________________________________________________________________ 1 Executive Summary_______________________________________________________________ 3 1. Objectives__________________________________________________________________ 5 2. Background ________________________________________________________________ 5 3. Method ____________________________________________________________________ 8 4. Analysis __________________________________________________________________ 10 5. Strategic model for increasing native woodland in the Scottish Borders _________________ 13 6. Identifying and managing the development of Forest Habitat Networks in the Scottish Borders _________________________________________________________________________ 17 7. The effect of Forest Habitat Network development on the Scottish Borders landscape. _____ 26 8. Conclusions _______________________________________________________________ 39 9. References ________________________________________________________________ 41 2 Executive Summary 1. This report describes a GIS based desk study to identify the semi-natural woodland framework for the development of a Native Woodland Habitat Network in the Scottish
    [Show full text]
  • Daer Wind Farm, South Lanarkshire/ Dumfries & Galloway
    Landscape Character Type: Project: 66. Agricultural Lowlands - Ayrshire 68. Lowland River Valleys - Ayrshire Daer Wind Farm, 69. Upland River Valleys - Ayrshire 73. Upland Glen - Ayrshire South Lanarkshire/ 74. Upland Basin - Ayrshire 76. Foothills - Ayrshire 78. Plateau Moorland - Ayrshire Dumfries & Galloway 81. Southern Uplands - Ayrshire 82. Southern Uplands with Forest - Ayrshire Title: 90. Dissected Plateau Moorland 92. Plateau Outliers Figure 5.5 Landscape Character 93. Southern Uplands with Scattered Forest - Borders 94. Rolling Moorland 95. Southern Uplands - Borders Key 96. Southern Uplands with Forest - Borders 99. Rolling Farmland - Borders Proposed turbine 101. Rocky Upland Fringe 102. Upland Fringe with Prominent Hills Distance from outermost turbines 113. Upland Valley with Pastoral Floor 114. Pastoral Upland Valley Viewpoint 116. Upland Valley with Woodland 117. Pastoral Upland Fringe Valley Local Authority boundary 158. Coastal Flats - Dumfries & Galloway 160. Narrow Wooded River Valley - Dumfries & Galloway Landscape Character Area by Region 161. Pastoral Valley - Dumfries & Galloway 162. Lower Dale - Dumfries & Galloway Glasgow & Clyde Valley (South Lanarkshire) 163. Middle Dale - Dumfries & Galloway 164. Flooded Valley Dumfries & Galloway 165. Upper Dale - Dumfries & Galloway 166. Upland Glens - Dumfries & Galloway Scottish Borders 169. Drumlin Pastures 170. Coastal Plateau - Dumfries & Galloway East Ayrshire 171. Flow Plateau 172. Upland Fringe - Dumfries & Galloway Theoretical number of turbines visible to tip height 175. Foothills - Dumfries & Galloway 176. Foothills with Forest - Dumfries & Galloway 1 - 3 177. Southern Uplands - Dumfries & Galloway 178. Southern Uplands with Forest - Dumfries & Galloway 4 - 6 179. Coastal Uplands 180. Rugged Uplands - Dumfries & Galloway 200. Rolling Farmland - Glasgow & Clyde Valley 7 - 10 201. Plateau Farmland - Glasgow & Clyde Valley 204. Incised River Valleys 11 - 14 207.
    [Show full text]