Zobrazeno 1 - 10
of 42
pro vyhledávání: '"T. M. L. WIGLEY"'
Publikováno v:
Geoscientific Model Development, Vol 10, Pp 2495-2524 (2017)
Sea level rise (SLR) is one of the major impacts of global warming; it will threaten coastal populations, infrastructure, and ecosystems around the globe in coming centuries. Well-constrained sea level projections are needed to estimate future los
Externí odkaz:
https://doaj.org/article/7a51145fb842478682c76d538cd99158
Publikováno v:
Atmospheric Chemistry and Physics, Vol 11, Iss 4, Pp 1457-1471 (2011)
Intercomparisons of coupled atmosphere-ocean general circulation models (AOGCMs) and carbon cycle models are important for galvanizing our current scientific knowledge to project future climate. Interpreting such intercomparisons faces major challeng
Externí odkaz:
https://doaj.org/article/1fef7bbfbdef4a34b7bd3dcd48c7e56f
Publikováno v:
Atmospheric Chemistry and Physics, Vol 11, Iss 4, Pp 1417-1456 (2011)
Current scientific knowledge on the future response of the climate system to human-induced perturbations is comprehensively captured by various model intercomparison efforts. In the preparation of the Fourth Assessment Report (AR4) of the Intergovern
Externí odkaz:
https://doaj.org/article/e07cb661103d47c4ad248d899de4650c
Publikováno v:
Hydrology and Earth System Sciences, Vol 4, Iss 3, Pp 355-371 (2000)
The classical one-dimensional advection-diffusion equation (ADE) gives an inadequate description of tracer cloud evolution in the River Severn, U.K. A solute transport model incorporating the effects of tracer storage in dead zones is presented in wh
Externí odkaz:
https://doaj.org/article/6aa65c3ee5c345d092e31046026ab1cb
Autor:
T. M. L. Wigley, D. S. Schimel
Reducing carbon dioxide (CO2) emissions is imperative to stabilizing our future climate. Our ability to reduce these emissions combined with an understanding of how much fossil-fuel-derived CO2 the oceans and plants can absorb is central to mitigatin
Autor:
B. D. Santer, P. W. Thorne, L. Haimberger, K. E. Taylor, T. M. L. Wigley, J. R. Lanzante, S. Solomon, M. Free, P. J. Gleckler, P. D. Jones, T. R. Karl, S. A. Klein, C. Mears, D. Nychka, G. A. Schmidt, S. C. Sherwood, F. J. Wentz
Publikováno v:
Climate Modelling ISBN: 9783319650579
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f0a269e3e89f8dd9871f123bbfc5c5a
https://doi.org/10.1007/978-3-319-65058-6_5
https://doi.org/10.1007/978-3-319-65058-6_5
Autor:
T. M. L. Wigley
Publikováno v:
Global Biogeochemical Cycles. 5:373-382
The convolution integral form of a carbon cycle model is transformed to a simple first-order differential equation. This allows one to derive an extremely efficient numerical algorithm for the carbon cycle model. The algorithm can be easily inverted
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38feb442224f8b4b9ad15ab8864d0541
https://doi.org/10.1029/91gb02279
https://doi.org/10.1029/91gb02279
Publikováno v:
Nature. 439(7077)
We have analysed a suite of 12 state-of-the-art climate models and show that ocean warming and sea-level rise in the twentieth century were substantially reduced by the colossal eruption in 1883 of the volcano Krakatoa in the Sunda strait, Indonesia.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::8a7d5c1a8218f202d54ff1ed242d780c
https://pubmed.ncbi.nlm.nih.gov/16467829
https://pubmed.ncbi.nlm.nih.gov/16467829