Zobrazeno 1 - 10
of 13
pro vyhledávání: '"L D Rotstayn"'
Publikováno v:
Environmental Research Letters, Vol 10, Iss 4, p 044018 (2015)
All of the representative concentration pathways (RCPs) assume that future emissions of aerosols and aerosol precursors will decline sharply. There is considerable evidence that historically increasing aerosols have substantially affected tropical pr
Externí odkaz:
https://doaj.org/article/2ad8375cad57433eb82d411399bbe419
Publikováno v:
Environmental Research Letters, Vol 8, Iss 1, p 014030 (2013)
We use single-forcing historical simulations with a coupled atmosphere–ocean global climate model to compare the effects of anthropogenic aerosols (AAs) and increasing long-lived greenhouse gases (LLGHGs) on simulated winter circulation in the Sout
Externí odkaz:
https://doaj.org/article/e1e372ca05e9411ea4b6cbddfee10461
Publikováno v:
Atmospheric Chemistry and Physics, Vol 13, Iss 21, Pp 10883-10905 (2013)
All the representative concentration pathways (RCPs) include declining aerosol emissions during the 21st century, but the effects of these declines on climate projections have had little attention. Here we assess the global and hemispheric-scale effe
Externí odkaz:
https://doaj.org/article/ea18fc1be9de4400b40507c25af41952
Autor:
A. Chrastansky, L. D. Rotstayn
Publikováno v:
Atmospheric Chemistry and Physics, Vol 12, Iss 23, Pp 11395-11416 (2012)
Emissions of biomass-burning aerosols from the Indonesian region are known to vary in response to rainfall anomalies associated with the El Niño Southern Oscillation (ENSO). For the severe El Niño-related drought in 1997, there have been several at
Externí odkaz:
https://doaj.org/article/2fbd43105f2347ff8e76ecc7c7d50e32
Autor:
L. D. Rotstayn, S. J. Jeffrey, M. A. Collier, S. M. Dravitzki, A. C. Hirst, J. I. Syktus, K. K. Wong
Publikováno v:
Atmospheric Chemistry and Physics, Vol 12, Iss 14, Pp 6377-6404 (2012)
We use a coupled atmosphere-ocean global climate model (CSIRO-Mk3.6) to investigate the drivers of trends in summer rainfall and circulation in the vicinity of northern Australia. As part of the Coupled Model Intercomparison Project Phase 5 (CMIP5),
Externí odkaz:
https://doaj.org/article/72e6cbd891444d0f8241692da9ee02f3
Publikováno v:
Geoscientific Model Development, Vol 5, Iss 3, Pp 649-682 (2012)
The CSIRO Mk3L climate system model is a coupled general circulation model, designed primarily for millennial-scale climate simulation and palaeoclimate research. Mk3L includes components which describe the atmosphere, ocean, sea ice and land surface
Externí odkaz:
https://doaj.org/article/1e8a338df3aa4beb87a7738072669267
Publikováno v:
Atmospheric Chemistry and Physics, Vol 11, Iss 13, Pp 6575-6592 (2011)
Australian dust emissions are highly episodic, and this may increase the importance of Australian dust as a climate feedback agent. We compare two 160-year coupled atmosphere-ocean simulations of modern-day climate using the CSIRO Mark 3.6 global cli
Externí odkaz:
https://doaj.org/article/d7f98d3db2094fbb9e0ee9a625a8706e
Publikováno v:
Geoscientific Model Development, Vol 4, Iss 2, Pp 483-509 (2011)
The CSIRO Mk3L climate system model is a coupled general circulation model, designed primarily for millennial-scale climate simulations and palaeoclimate research. Mk3L includes components which describe the atmosphere, ocean, sea ice and land surfac
Externí odkaz:
https://doaj.org/article/410c27496e28441e9a7915e85e164992
Publikováno v:
Atmospheric Chemistry and Physics, Vol 12, Iss 3, Pp 1481-1481 (2012)
No abstract available.
Externí odkaz:
https://doaj.org/article/920cb9717ddd4e8bb10fbec20d553bc1
