Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Hilary Spencer"'
Autor:
Hilary Spencer, Joel Smith, Anna Jones, Jane Williams, Deborah Gill, Rosie Belcher, Tim Vincent, William Coppola, Chris Cooper, Julia Montgomery, Alex Haig, Laura-Jane Smith, Inam Haq, Nigel Rawlinson
Publikováno v:
The Clinical Teacher. 11:546-550
BACKGROUND: As the health care education landscape in the UK changes rapidly and dramatically, collaboration across institutions bridging undergraduate and postgraduate fields is increasingly necessary. Collaboration entails both risks and benefits.
Publikováno v:
Academic Medicine. 84:1003-1007
The practice of clinical medicine is becoming increasingly specialized, and this change has increased the challenge of developing fair, valid, and reliable tests of knowledge, particularly for single candidates or small groups of candidates. The prob
Publikováno v:
Journal of Climate. 20:2273-2298
Here the factors affecting the mean state and El Niño variability in the Third Hadley Centre Coupled Ocean–Atmosphere General Circulation Model (HadCM3) are examined with and without heat flux or wind stress corrections. There is currently little
Autor:
Helene T. Banks, Alejandro Bodas-Salcedo, Buwen Dong, William Ingram, Anne Pardaens, Jonathan M. Gregory, Jeff Ridley, A. J. McLaren, S. Cusack, Graham J. Rickard, Hilary Spencer, Keith D. Williams, T. C. Johns, Michel Crucifix, Jason Lowe, C. F. Durman, Richard Hill, David M. H. Sexton, Catherine A. Senior, A. B. Keen, Manoj Joshi, Y. Searl, Malcolm J. Roberts, Sheila Stark, A. K. Jones
Publikováno v:
ResearcherID
A new coupled general circulation climate model developed at the Met Office's Hadley Centre is presented, and aspects of its performance in climate simulations run for the Intergovernmental Panel on Climate Change Fourth Assessment Report (IPCC AR4)
Publikováno v:
ResearcherID
Prediction of Indian Ocean interannual variability may be limited by the systematic biases in coupled GCMs or by a lack of resolution of the processes involved. In particular, little is known about the impact of ocean resolution on simulated climate
Publikováno v:
Climate Dynamics. 22:511-526
In this modelling study, the teleconnections of ENSO are studied using an atmospheric general circulation model (AGCM), HadAM3. The influence of sea surface temperature anomalies (SSTAs) remote from the tropical Pacific but teleconnected with ENSO is
Autor:
Hilary Spencer, Julia Slingo
Publikováno v:
Journal of Climate. 16:1757-1774
There is much evidence that El Nino and La Nina lead to significant atmospheric seasonal predictability across much of the globe. However, despite successful predictions of tropical Pacific SSTs, atmospheric seasonal forecasts have had limited succes
Publikováno v:
Journal of Climate
Journal of Climate, 2006, 19 (9), pp.1850-1868. ⟨10.1175/JCLI3706.1⟩
Journal of Climate, American Meteorological Society, 2006, 19 (9), pp.1850-1868. ⟨10.1175/JCLI3706.1⟩
ResearcherID
Journal of Climate, 2006, 19 (9), pp.1850-1868. ⟨10.1175/JCLI3706.1⟩
Journal of Climate, American Meteorological Society, 2006, 19 (9), pp.1850-1868. ⟨10.1175/JCLI3706.1⟩
ResearcherID
In this study, the mechanisms leading to the El Niño peak and demise are explored through a coupled general circulation model ensemble approach evaluated against observations. The results here suggest that the timing of the peak and demise for inten
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1992c4372d432db7b73398666c3eff0c
https://hal.science/hal-00124667/document
https://hal.science/hal-00124667/document
Publikováno v:
ResearcherID
This paper reviews the meteorology of the Western Indian Ocean and uses a state–of–the–art atmospheric general circulation model to investigate the influence of the East African Highlands on the climate of the Indian Ocean and its surrounding r
Autor:
Hilary Spencer
Publikováno v:
Geophysical Research Letters. 31
[1] The variations with the seasonal cycle of the atmospheric response to constant SST anomalies in the eastern tropical Pacific are investigated with the atmospheric GCM, HadAM3. The equatorial wind response is weakest in January and February when t