Gotowe bibliografie tematyczne / Meteorology, climatic change, Australia, temperature

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Gotowa bibliografia na temat „Meteorology, climatic change, Australia, temperature”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 3 lutego 2022

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Artykuły w czasopismach na temat "Meteorology, climatic change, Australia, temperature"

Hudson, Debra, Oscar Alves, Harry H. Hendon, Eun-Pa Lim, Guoqiang Liu, Jing-Jia Luo, Craig MacLachlan, et al. "ACCESS-S1 The new Bureau of Meteorology multi-week to seasonal prediction system." Journal of Southern Hemisphere Earth Systems Science 67, no. 3 (2017): 132. http://dx.doi.org/10.1071/es17009.

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ACCESS-S1 will be the next version of the Australian Bureau of Meteorology's seasonal prediction system, due to become operational in early 2018. The multiweek and seasonal performance of ACCESS-S1 has been evaluated based on a 23-year hindcast set and compared to the current operational system, POAMA. The system has considerable enhancements compared to POAMA, including higher vertical and horizontal resolution of the component models and state-ofthe-art physics parameterisation schemes. ACCESS-S1 is based on the UK Met Office GloSea5-GC2 seasonal prediction system, but has enhancements to th

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Hudson, Debra, Oscar Alves, Harry H. Hendon, Eun-Pa Lim, Guoqiang Liu, Jing-Jia Luo, Craig MacLachlan, et al. "Corrigendum to: ACCESS-S1: The new Bureau of Meteorology multi-week to seasonal prediction system." Journal of Southern Hemisphere Earth Systems Science 70, no. 1 (2020): 393. http://dx.doi.org/10.1071/es17009_co.

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Bettio, Lynette, John R. Nairn, Steven C. McGibbony, Pandora Hope, Andrew Tupper, and Robert J. B. Fawcett. "A heatwave forecast service for Australia." Proceedings of the Royal Society of Victoria 131, no. 1 (2019): 53. http://dx.doi.org/10.1071/rs19006.

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The Australian Bureau of Meteorology monitors, researches, predicts and communicates Australia’s weather and climate. Australia’s mean temperature has risen by over 1°C since 1910, leading to an increase in the frequency of extreme heat events. Extreme heat can profoundly impact human health, infrastructure and the environment. Research conducted at the Bureau and elsewhere shows that climate change is impacting the intensity and frequency of extreme heat events. One way that the Bureau has responded to this challenge is by providing a forecast service specifically targeted at identifying heat

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Hartigan, Joshua, Shev MacNamara, and Lance M. Leslie. "Comparing precipitation and temperature trends between inland and coastal locations." ANZIAM Journal 60 (July 17, 2019): C109—C126. http://dx.doi.org/10.21914/anziamj.v60i0.13967.

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Motivated by the Millennium Drought and the current drought over much of southern and eastern Australia, this detailed statistical study compares trends in annual wet season precipitation and temperature between a coastal site (Newcastle) and an inland site (Scone). Bootstrap permutation tests reveal Scone precipitation has decreased significantly over the past 40 years (p-value=0.070) whereas Newcastle has recorded little to no change (p-value=0.800). Mean maximum and minimum temperatures for Newcastle have increased over the past 40 years (p-values of 0.002 and 0.015, respectively) while the

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Ly, Pham Thi, and Hoang Luu Thu Thuy. "Spatial distribution of hot days in north central region, Vietnam in the period of 1980-2013." VIETNAM JOURNAL OF EARTH SCIENCES 41, no. 1 (January 8, 2019): 36–45. http://dx.doi.org/10.15625/0866-7187/41/1/13544.

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Based on the data of daily maximum temperature in 26 meteorological stations in the North Center Region, Vietnam over the period of 1980 to 2013, the authors conducted the research on the spatial distribution of the number of hot days. The initial result shows that in general, in the north of the study area, the large number of hot days occurred in the plain, and tended to decrease westward and eastward. In the south, this number tends to increase from the west to the east. Especially, the largest number occurred in two areas: The Ma and Ca River's valleys (Thanh Hoa and Nghe An provinces) and

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Shi, Li, Harry H. Hendon, Oscar Alves, Jing-Jia Luo, Magdalena Balmaseda, and David Anderson. "How Predictable is the Indian Ocean Dipole?" Monthly Weather Review 140, no. 12 (December 1, 2012): 3867–84. http://dx.doi.org/10.1175/mwr-d-12-00001.1.

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Abstract In light of the growing recognition of the role of surface temperature variations in the Indian Ocean for driving global climate variability, the predictive skill of the sea surface temperature (SST) anomalies associated with the Indian Ocean dipole (IOD) is assessed using ensemble seasonal forecasts from a selection of contemporary coupled climate models that are routinely used to make seasonal climate predictions. The authors assess predictions from successive versions of the Australian Bureau of Meteorology Predictive Ocean–Atmosphere Model for Australia (POAMA 15b and 24), success

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Griesser, A. G., and C. M. Spillman. "Assessing the Skill and Value of Seasonal Thermal Stress Forecasts for Coral Bleaching Risk in the Western Pacific." Journal of Applied Meteorology and Climatology 55, no. 7 (July 2016): 1565–78. http://dx.doi.org/10.1175/jamc-d-15-0109.1.

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AbstractOver the last 30 years, coral reefs around the world have been under considerable stress because of increasing anthropogenic pressures, overfishing, pollution, and climate change. A primary stress factor is anomalously warm water events, which can cause mass coral bleaching and widespread reef damage. Forecasts of sea surface temperature (SST) and the associated risk of coral bleaching can assist managers, researchers, and other stakeholders in monitoring and managing coral reef resources. At the Australian Bureau of Meteorology, monthly forecasts of SST and thermal stress metrics have

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Zhang, Lifu, Na Qiao, Changping Huang, and Siheng Wang. "Monitoring Drought Effects on Vegetation Productivity Using Satellite Solar-Induced Chlorophyll Fluorescence." Remote Sensing 11, no. 4 (February 13, 2019): 378. http://dx.doi.org/10.3390/rs11040378.

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Around the world, the increasing drought, which is exacerbated by climate change, has significant impacts on vegetation carbon assimilation. Identifying how short-term climate anomalies influence vegetation productivity in a timely and accurate manner at the satellite scale is crucial to monitoring drought. Satellite solar-induced chlorophyll fluorescence (SIF) has recently been reported as a direct proxy of actual vegetation photosynthesis and has more advantages than traditional vegetation indices (e.g., the Normalized Difference Vegetation Index, NDVI and the Enhanced Vegetation Index, EVI)

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Verbeke, T., J. Lathière, S. Szopa, and N. de Noblet-Ducoudré. "Impact of future land-cover changes on HNO3 and O3 surface dry deposition." Atmospheric Chemistry and Physics 15, no. 23 (December 9, 2015): 13555–68. http://dx.doi.org/10.5194/acp-15-13555-2015.

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Abstract. Dry deposition is a key component of surface–atmosphere exchange of compounds, acting as a sink for several chemical species. Meteorological factors, chemical properties of the trace gas considered and land surface properties are strong drivers of dry deposition efficiency and variability. Under both climatic and anthropogenic pressure, the vegetation distribution over the Earth has been changing a lot over the past centuries and could be significantly altered in the future. In this study, we perform a modeling investigation of the potential impact of land-cover changes between the p

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Broich, M., and M. G. Tulbure. "RESPONSE OF RIPARIAN VEGETATION IN AUSTRALIA"S LARGEST RIVER BASIN TO INTER AND INTRA-ANNUAL CLIMATE VARIABILITY AND FLOODING AS QUANTIFIED WITH LANDSAT AND MODIS." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLI-B8 (June 23, 2016): 577–78. http://dx.doi.org/10.5194/isprs-archives-xli-b8-577-2016.

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Australia is a continent subject to high rainfall variability, which has major influences on runoff and vegetation dynamics. However, the resulting spatial-temporal pattern of flooding and its influence on riparian vegetation has not been quantified in a spatially explicit way. Here we focused on the floodplains of the entire Murray-Darling Basin (MDB), an area that covers over 1M&thinsp;km2, as a case study. The MDB is the country’s primary agricultural area with scarce water resources subject to competing demands and impacted by climate change and more recently by

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Rozprawy doktorskie na temat "Meteorology, climatic change, Australia, temperature"

Torok, Simon James. "The development of a high quality historical temperature data base for Australia." 1996. http://repository.unimelb.edu.au/10187/2407.

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A high quality, historical surface air temperature data set is essential for the reliable investigation of climate change and variability. In this study, such a data set has been prepared for Australia by adjusting raw mean annual temperature data for inhomogeneities associated with station relocations, changes in exposure, and other problems. Temperature records from long-term stations were collaborated from the set of all raw data held by the Australian Bureau of Meteorology. These long-term records were extended by combining stations and manually entering previously unused archived temperat

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Pattanayak, Sonali. "A Hydroclimatological Change Detection and Attribution Study over India using CMIP5 Models." Thesis, 2015. http://etd.iisc.ernet.in/handle/2005/2761.

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As a result of increase in global average surface temperature, abnormalities in different hydroclimatic components such as evapotranspiration, stream flow and precipitation have been experienced. So investigation has to be carried out to assess the hidden abnormality subsisting in the hydroclimatological time series in the form of trend. This thesis broadly consists of following four parts. The first part comprises of a detailed review of various trend detection approaches. Approaches incorporating the effect of serial correlation for trend detection and interesting developments concerning var

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Książki na temat "Meteorology, climatic change, Australia, temperature"

Eddy, Richard L. Variability of wet and dry periods in the Upper Colorado River Basin and the possible effects of climate change and sensitivity of probable maximum precipitation estimates to climate change. Denver, Colo: U.S. Dept. of the Interior, Bureau of Reclamation, Denver Office, 1996.

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The warming papers: The scientific foundation for the climate change forecast. Hoboken: Wiley-Blackwell, 2011.

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Grotch, Stanley L. An intercomparison of general circulation model predictions of regional climate change: Presented at the International Conference on "Modelling of Global Climate Change and Variability," Hamburg, Federal Republic of Germany, September 1989. [Springfield, Va: Available from National Technical Information Service, 1990.

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United States. Congress. House. Committee on Science, Space, and Technology. Subcommittee on Natural Resources, Agriculture Research, and Environment. The National Climate Program Act and global climate change: Hearings before the Subcommittee on Natural Resources, Agriculture Research, and Environment and the Subcommittee on International Scientific Cooperation of the Committee on Science, Space, and Technology, U.S. House of Representatives, One Hundredth Congress, first session, July 22, 23, 29; September 30, 1987. Washington: U.S. G.P.O., 1988.

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Library of Congress. Congressional Research Service. and United States. Congress. Senate. Committee on Agriculture, Nutrition, and Forestry., eds. Agriculture, forestry, and global climate change--a reader. Washington: U.S. G.P.O., 1989.

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Trends '93: A compendium of data on global change. Oak Ridge, Tenn: Carbon Dioxide Information Analysis Center, World Data Center-A for Atmospheric Trace Gases, Environmental Sciences Division, Oak Ridge National Laboratory, 1994.

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Shu, Geng, Cady Casey Walsh, and University of California Pacific Rim Program., eds. Climatic variation and change: Implications for agriculture in the Pacific Rim : proceedings : conferences held June 20-28, 1989, University of California, Davis, USA [and] September 24-28, 1990, University of Melbourne, Australia. Davis: Public Service Research and Dissemination Program, University of California, Davis, 1991.

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Części książek na temat "Meteorology, climatic change, Australia, temperature"

Buckley, B. M., E. R. Cook, M. J. Peterson, and M. Barbetti. "A Changing Temperature Response with Elevation for Lagarostrobos Franklinii in Tasmania, Australia." In Climatic Change at High Elevation Sites, 245–66. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-015-8905-5_13.

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Fleming, James R. "John Tyndall, Svante Arrhenius, and Early Research on Carbon Dioxide and Climate." In Historical Perspectives on Climate Change. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195078701.003.0011.

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In the second half of the nineteenth century two prominent scientists, working in two distinct specialties, identified the importance of atmospheric trace constituents as efficient absorbers of long-wave radiation and as factors in climatic control. John Tyndall conducted the first convincing experiments on the radiative properties of gases, demonstrating that “perfectly colorless and invisible gases and vapours” were able to absorb and emit radiant heat. Svante Arrhenius, in pursuing his interests in meteorology and cosmic physics, demonstrated that variations of atmospheric CO2 concentration could have a very great effect on the overall heat budget and surface temperature of the planet. It would be a mistake, however, to consider either of these individuals as direct forerunners or prophets of contemporary climate concerns. Each of them had extremely broad scientific interests and pursued climate-related research as one interest among many. Tyndall worked on absorption in the near infrared at temperatures far above those of the terrestrial environment. Arrhenius, who has recently gained renewed attention as the “father” of the theory of the greenhouse effect, held assumptions and produced results that are not continuous with present-day climate research. . . . The solar heat possesses, in a far higher degree than that of lime light, the power of crossing an atmosphere; but, when the heat is absorbed by the planet, it is so changed in quality that the rays emanating from the planet cannot get with the same freedom back into space. Thus the atmosphere admits of the entrance of the solar heat, but checks its exit; and the result is a tendency to accumulate heat at the surface of the planet. —John Tyndall (1859). . . John Tyndall was born in Leighlin Bridge, County Carlow, Ireland, on August 2, 1820, the son of a part-time shoemaker and constable. He attended the national school in Carlow and, at the age of eighteen, joined the Irish Ordnance Survey as a draftsman and surveyor. In 1842, as the Irish survey neared completion, Tyndall was transferred to the English Survey at Preston, Lancashire, but due to his protests against the survey’s oppressive policies and incompetent management, he was dismissed.

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