Your selections:
Massively multiplayer online role-playing games : The past, present, and future
- Achterbosch, Leigh, Pierce, Robyn, Simmons, Gregory
A taxonomy of griefer type by motivation in massively multiplayer online role-playing games
- Achterbosch, Leigh, Miller, Charlynn, Vamplew, Peter
Griefers versus the Griefed - what motivates them to play Massively Multiplayer Online Role-Playing Games?
- Achterbosch, Leigh, Miller, Charlynn, Turville, Christopher, Vamplew, Peter
Evaluation of PMIP2 and PMIP3 simulations of mid-Holocene climate in the Indo-Pacific, Australasian and Southern Ocean regions
- Ackerley, Duncan, Reeves, Jessica, Barr, Cameron, Bostock, Helen, Fitzsimmons, Kathryn, Fletcher, Michael-Shawn, Gouramanis, Chris, McGregor, Helen, Mooney, Scott, Phipps, Steven, Tibby, John, Tyler, Jonathan
simplified patterns of temperature and effective precipitationapproach from the Australian component of the international palaeoclimate synthesis effort (INTegration of Ice core, MArine and TErrestrial records - OZ-INTIMATE) to compare atmosphere-ocean general circulation model (AOGCM) simulations and proxy reconstructions. The approach is used in order to identify important properties (e.g. circulation and precipitation) of past climatic states from the models and proxies, which is a primary objective of the Southern Hemisphere Assessment of PalaeoEnvironment (SHAPE) initiative. The AOGCM data are taken from the Paleoclimate Modelling Intercomparison Project (PMIP) mid-Holocene (ca. 6000 years before present, 6 ka) and pre-industrial control (ca. 1750 CE, 0 ka) experiments. The synthesis presented here shows that the models and proxies agree on the differences in climate state for 6 ka relative to 0 ka, when they are insolation driven. The largest uncertainty between the models and the proxies occurs over the Indo-Pacific Warm Pool (IPWP). The analysis shows that the lower temperatures in the Pacific at around 6 ka in the models may be the result of an enhancement of an existing systematic error. It is therefore difficult to decipher which one of the proxies and/or the models is correct. This study also shows that a reduction in the Equator-to-pole temperature difference in the Southern Hemisphere causes the mid-latitude westerly wind strength to reduce in the models; however, the simulated rainfall actually increases over the southern temperate zone of Australia as a result of higher convective precipitation. Such a mechanism (increased convection) may be useful for resolving disparities between different regional proxy records and model simulations. Finally, after assessing the available datasets (model and proxy), opportunities for better model-proxy integrated research are discussed. © Author(s) 2017.
simplified patterns of temperature and effective precipitationapproach from the Australian component of the international palaeoclimate synthesis effort (INTegration of Ice core, MArine and TErrestrial records - OZ-INTIMATE) to compare atmosphere-ocean general circulation model (AOGCM) simulations and proxy reconstructions. The approach is used in order to identify important properties (e.g. circulation and precipitation) of past climatic states from the models and proxies, which is a primary objective of the Southern Hemisphere Assessment of PalaeoEnvironment (SHAPE) initiative. The AOGCM data are taken from the Paleoclimate Modelling Intercomparison Project (PMIP) mid-Holocene (ca. 6000 years before present, 6 ka) and pre-industrial control (ca. 1750 CE, 0 ka) experiments. The synthesis presented here shows that the models and proxies agree on the differences in climate state for 6 ka relative to 0 ka, when they are insolation driven. The largest uncertainty between the models and the proxies occurs over the Indo-Pacific Warm Pool (IPWP). The analysis shows that the lower temperatures in the Pacific at around 6 ka in the models may be the result of an enhancement of an existing systematic error. It is therefore difficult to decipher which one of the proxies and/or the models is correct. This study also shows that a reduction in the Equator-to-pole temperature difference in the Southern Hemisphere causes the mid-latitude westerly wind strength to reduce in the models; however, the simulated rainfall actually increases over the southern temperate zone of Australia as a result of higher convective precipitation. Such a mechanism (increased convection) may be useful for resolving disparities between different regional proxy records and model simulations. Finally, after assessing the available datasets (model and proxy), opportunities for better model-proxy integrated research are discussed. © Author(s) 2017.
Hip and knee osteoarthritis affects younger people, too
- Ackerman, Ilana, Kemp, Joanne, Crossley, Kay, Culvenor, Adam, Hinman, Rana
Assessing health risk of reclaimed water using human cell culture
- Ackland, Margaret, Michalczyk, Agnes, Freestone, David, Stagnitti, Frank
- Adair, Tim, Lourey, Emma, Taylor, Philip
- Adak, Dibyendu, Pramod, ALN, Ooi, Ean Tat, Natarajan, Sundararajan
On optimal control of a sweeping process coupled with an ordinary differential equation
- Adams, Maria, Law, Bradley, Gibson, Matthew
Representing militancy: photographs of the Broken Hill industrial disputes, 1908-20
Political imaginaries in question
- Adams, Suzi, Smith, Jeremy, Straume, Ingerid
Recalling childhood : transformative learning about the value of play through active participation
- Adamson, Gracie, Rouse, Elizabeth, Emmett, Susan
Phosphorus distribution in soils from Australian dairy and beef rearing pastoral systems
- Adeloju, Samuel, Webb, Benjamin, Smernik, Ronald
The association between selected molecular biomarkers and ambulatory blood pressure patterns in African chronic kidney disease and hypertensive patients compared with normotensive controls : protocol for a longitudinal study
- Adeoye, Abiodun, Adebayo, Oladimeji, Abiola, Busayo, Iwalokun, Bamidele, Tayo, Bamidele, Charchar, Fadi, Ojo, Akinlolu, Cooper, Richard
- Adhikari, Benu, Howes, Tony, Bhandari, Bhesh, Truong, V.
The effect of low molecular weight surfactants and proteins on surface stickiness of sucrose during powder formation through spray drying
- Adhikari, Benu, Howes, Tony, Wood, B. J., Bhandari, Bhesh
Characterization of the surface stickiness of fructose-maltodextrin solutions during drying
- Adhikari, Benu, Howes, Tony, Bhandari, Bhesh, Truong, V.
Effect of plasticizers on the moisture migration behavior of low-amylose starch films during drying
- Adhikari, Benu, Chaudhary, Deeptangshu, Clerfeuille, E
Thin-layer isothermal drying of fructose, maltodextrin, and their mixture solutions
- Adhikari, Benu, Howes, Tony, Shrestha, A., Tsai, W., Bhandari, Bhesh
Are you sure you would like to clear your session, including search history and login status?