UK Climate Projections: Summer Daytime and Nighttime Urban Heat Island Changes in England's Major Cities

被引:28
作者
Lo, Y. T. Eunice [1 ]
Mitchell, Daniel M. [1 ]
Bohnenstengel, Sylvia, I [2 ]
Collins, Mat [3 ]
Hawkins, Ed [4 ,5 ]
Hegerl, Gabriele C. [6 ]
Joshi, Manoj [7 ]
Stott, Peter A. [3 ,8 ]
机构
[1] Univ Bristol, Sch Geog Sci, Bristol, Avon, England
[2] Univ Reading, Dept Meteorol, MetOff Reading, Reading, Berks, England
[3] Univ Exeter, Coll Engn Math & Phys Sci, Exeter, Devon, England
[4] Univ Reading, Natl Ctr Atmospher Sci, Reading, Berks, England
[5] Univ Reading, Dept Meteorol, Reading, Berks, England
[6] Univ Edinburgh, Sch Geosci, Edinburgh, Midlothian, Scotland
[7] Univ East Anglia, Sch Environm Sci, Climat Res Unit, Norwich, Norfolk, England
[8] Met Off Hadley Ctr, Exeter, Devon, England
关键词
Atmosphere-land interaction; Climate change; Temperature; Climate models; Trends;
D O I
10.1175/JCLI-D-19-0961.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In the United Kingdom, where 90% of residents are projected to live in urban areas by 2050, projecting changes in urban heat islands (UHIs) is essential to municipal adaptation. Increased summer temperatures are linked to increased mortality. Using the new regional U.K. Climate Projections, UKCP18-regional, we estimate the 1981-2079 trends in summer urban and rural near-surface air temperatures and in UHI intensities during day and at night in the 10 most populous built-up areas in England. Summer temperatures increase by 0.45 degrees-0.81 degrees C per decade under RCP8.5, depending on the time of day and location. Nighttime temperatures increase more in urban than rural areas, enhancing the nighttime UHI by 0.01 degrees-0.05 degrees C per decade in all cities. When these upward UHI signals emerge from 2008-18 variability, positive summer nighttime UHI intensities of up to 1.8 degrees C are projected in most cities. However, we can prevent most of these upward nighttime UHI signals from emerging by stabilizing climate to the Paris Agreement target of 2 degrees C above preindustrial levels. In contrast, daytime UHI intensities decrease in nine cities, at rates between -0.004 degrees and -0.05 degrees C per decade, indicating a trend toward a reduced daytime UHI effect. These changes reflect different feedbacks over urban and rural areas and are specific to UKCP18-regional. Future research is important to better understand the drivers of these UHI intensity changes.
引用
收藏
页码:9015 / 9030
页数:16
相关论文
共 76 条
  • [1] Urban heat island in a coastal urban area in northern Spain
    Acero, Juan A.
    Arrizabalaga, Jon
    Kupski, Sebastian
    Katzschner, Lutz
    [J]. THEORETICAL AND APPLIED CLIMATOLOGY, 2013, 113 (1-2) : 137 - 154
  • [2] Modeling of the urban heat island in the form of mesoscale wind and of its effect on air pollution dispersal
    Agarwal, Manju
    Tandon, Abhinav
    [J]. APPLIED MATHEMATICAL MODELLING, 2010, 34 (09) : 2520 - 2530
  • [3] Global to city scale urban anthropogenic heat flux: model and variability
    Allen, L.
    Lindberg, F.
    Grimmond, C. S. B.
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2011, 31 (13) : 1990 - 2005
  • [4] [Anonymous], 2015, Adoption of the Paris Agreement ‐ Paris Agreement text English
  • [5] Temperature response to future urbanization and climate change
    Argueeso, Daniel
    Evans, Jason P.
    Fita, Lluis
    Bormann, Kathryn J.
    [J]. CLIMATE DYNAMICS, 2014, 42 (7-8) : 2183 - 2199
  • [6] The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City
    Basara, Jeffrey B.
    Basara, Heather G.
    Illston, Bradley G.
    Crawford, Kenneth C.
    [J]. ADVANCES IN METEOROLOGY, 2010, 2010
  • [7] The Joint UK Land Environment Simulator (JULES), model description - Part 1: Energy and water fluxes
    Best, M. J.
    Pryor, M.
    Clark, D. B.
    Rooney, G. G.
    Essery, R. L. H.
    Menard, C. B.
    Edwards, J. M.
    Hendry, M. A.
    Porson, A.
    Gedney, N.
    Mercado, L. M.
    Sitch, S.
    Blyth, E.
    Boucher, O.
    Cox, P. M.
    Grimmond, C. S. B.
    Harding, R. J.
    [J]. GEOSCIENTIFIC MODEL DEVELOPMENT, 2011, 4 (03) : 677 - 699
  • [8] Representing urban areas within operational numerical weather prediction models
    Best, MJ
    [J]. BOUNDARY-LAYER METEOROLOGY, 2005, 114 (01) : 91 - 109
  • [9] Strong Dependence of Atmospheric Feedbacks on Mixed-Phase Microphysics and Aerosol-Cloud Interactions in HadGEM3
    Bodas-Salcedo, A.
    Mulcahy, J. P.
    Andrews, T.
    Williams, K. D.
    Ringer, M. A.
    Field, P. R.
    Elsaesser, G. S.
    [J]. JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, 2019, 11 (06): : 1735 - 1758
  • [10] Impact of anthropogenic heat emissions on London's temperatures
    Bohnenstengel, S. I.
    Hamilton, I.
    Davies, M.
    Belcher, S. E.
    [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2014, 140 (679) : 687 - 698