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Books on the topic 'Annual variability'

Author: Grafiati

Published: 25 May 2024

Last updated: 25 July 2025

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1

Rockcastle, Siobhan, and Marilyne Andersen. Annual Dynamics of Daylight Variability and Contrast. Springer London, 2013. http://dx.doi.org/10.1007/978-1-4471-5233-0.

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2

Yi, Chao, and United States. National Aeronautics and Space Administration., eds. Evolution dynamics of tropical ocean-atmosphere annual cycle variability. National Aeronautics and Space Administration, 1996.

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3

Quadir, Dewan Abdul. Inter-annual and intra-seasonal variability of temperature and precipitation of Bhutan. SAARC Meteorological Research Centre (SMRC), 2005.

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4

Furgerson, John Alan. Inter-annual variability of acoustic ray travel times in the Northeast Pacific. Available from the National Technical Information Service, 1990.

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5

P, Wilkerson Frances, and United States. National Aeronautics and Space Administration., eds. Global climatology and variability of potential new production estimated from remote sensing of sea-surface temperature: Final report. National Aeronautics and Space Administration, 1995.

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6

United States. National Aeronautics and Space Administration., ed. Assessment of climate variability of the Greenland Ice Sheet: Integration of in situ and satellite data. University of Colorado, Cooperative Institute for Research in Environmental Sciences, 1994.

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7

Eckermann, Stephen D. Mesoscale variability in SUCCESS data: Contract NAS5-97247 : annual report, Oct. 1, 1997-Sep 30, 1998. National Aeronautics and Space Administration, 1998.

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8

Hulme, M. The tropical easterly jet and Sudan rainfall 2: Inter- and intra-annual variability during 1968-85. University of Salford Department of Geography, 1988.

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9

United States. National Aeronautics and Space Administration., ed. Interannual variation of seasonal means and subseasonal variability of cloud streets off the east coast of North America, 1984-1987. Univ. of Northern Colorado, Geography Dept., 1990.

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10

Rockcastle, Siobhan. Annual Dynamics of Daylight Variability and Contrast: A Simulation-Based Approach to Quantifying Visual Effects in Architecture. Springer London, 2013.

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11

United States. National Aeronautics and Space Administration., ed. Coronal abundances and their variation: Annual progress report for contract NASW-4814. National Aeronautics and Space Administration, 1995.

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12

G, Bromage Timothy, and United States. National Aeronautics and Space Administration., eds. Quantification of bone growth rate variability in rats exposed to micro- (near zero G) and macrogravity (2G): Year 1 annual report. National Aeronautics and Space Administration, 1996.

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13

Pacific Climate Workshop (7th 1990 Asilomar, Calif.). Proceedings of the seventh annual Pacific Climate (PACLIM) Workshop, Asilomar, California--April 1990: Climate variability of the eastern North Pacific and western North America. Interagency Ecological Studies Program for the Sacramento-San Joaquin Estuary, 1991.

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14

Pacific Climate Workshop (8th 1991 Asilomar, Calif.). Proceedings of the eighth annual Pacific Climate (PACLIM) Workshop, Asilomar, California--March 10-13, 1991: Climate variability of the eastern North Pacific and western North America. Interagency Ecological Studies Program for the Sacramento-San Joaquin Estuary, 1992.

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15

L, Dryden I., Gill C. A, Mardia K. V, and Leeds Annual Statistical Research Workshop (16th : 1996 : Leeds, England), eds. Proceedings in image fusion and shape variability techniques: International conference, held in Leeds, UK, 3-5 July 1996, incorporating the 16th Leeds Annual Statistical Research (L.A.S.R.) Workshop ... Leeds University Press, 1996.

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16

Pacific Climate Workshop (18th 2001 Asilomar Conference Grounds). Proceedings of the Eighteenth Annual Pacific Climate Workshop: Asilomar Conference Grounds, Pacific Grove, California, March 18-21, 2001 : climate variability of the eastern North Pacific and western North America. Interagency Ecological Program for the Sacramento-San Joaquin Estuary, 2002.

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17

France, Collège de. Gènes et culture: Enveloppe génétique et variabilité culturelle. Symposium annuel. Jacob, 2003.

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18

Annual Dynamics Of Daylight Variability And Contrast A Simulationbased Approach To Quantifying Visual Effects In Architecture. Springer London Ltd, 2013.

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19

Mesoscale variability in SUCCESS data: Contract NAS5-97247 : annual report, Oct. 1, 1997-Sep 30, 1998. National Aeronautics and Space Administration, 1998.

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20

Simulated Annual and Seasonal Arctic Ocean and Sea-Ice Variability From a High Resolution, Coupled Ice-Ocean Model. Storming Media, 2001.

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21

Townsend, Simon, Dina Makarynska, and Julia Schult. Developing an Integrated Long-Term Monitoring Program for Darwin Harbour : Water Quality Pilot Project WP2: Intra-Annual Water Quality Variability. Northern Territory Government - Department of Environment and Natural Resources, 2019.

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22

Coronal abundances and their variation: Annual progress report for contract NASW-4814. National Aeronautics and Space Administration, 1995.

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23

Quantification of bone growth rate variability in rats exposed to micro- (near zero G) and macrogravity (2G): Year 1 annual report. National Aeronautics and Space Administration, 1996.

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24

Coronal abundances and their variation: Semi-annual progress report for contract NASW-d814. National Aeronautics and Space Administration, 1993.

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25

Goswami, B. N., and Soumi Chakravorty. Dynamics of the Indian Summer Monsoon Climate. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.613.

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Lifeline for about one-sixth of the world’s population in the subcontinent, the Indian summer monsoon (ISM) is an integral part of the annual cycle of the winds (reversal of winds with seasons), coupled with a strong annual cycle of precipitation (wet summer and dry winter). For over a century, high socioeconomic impacts of ISM rainfall (ISMR) in the region have driven scientists to attempt to predict the year-to-year variations of ISM rainfall. A remarkably stable phenomenon, making its appearance every year without fail, the ISM climate exhibits a rather small year-to-year variation (the sta

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26

Nash, David. Changes in Precipitation Over Southern Africa During Recent Centuries. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.539.

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Precipitation levels in southern Africa exhibit a marked east–west gradient and are characterized by strong seasonality and high interannual variability. Much of the mainland south of 15°S exhibits a semiarid to dry subhumid climate. More than 66 percent of rainfall in the extreme southwest of the subcontinent occurs between April and September. Rainfall in this region—termed the winter rainfall zone (WRZ)—is most commonly associated with the passage of midlatitude frontal systems embedded in the austral westerlies. In contrast, more than 66 percent of mean annual precipitation over much of th

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27

Lovejoy, Shaun. Weather, Macroweather, and the Climate. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190864217.001.0001.

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Weather, Macroweather, and the Climate is an insider's attempt to explain as simply as possible how to understand the atmospheric variability that occurs over an astonishing range of scales: from millimeters to the size of the planet, from milliseconds to billions of years. The variability is so large that standard ways of dealing with it are utterly inadequate: in 2015, it was found that classical approaches had underestimated the variability by the astronomical factor of a quadrillion (a million billion). Author Shaun Lovejoy asks - and answers - many fundamental questions such as: Is the at

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28

Burton, Derek, and Margaret Burton. Reproduction. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198785552.003.0009.

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Interspecific fish reproductive patterns, outputs and life cycles display the greatest variability within the vertebrates. Early stages of oogenesis can be repeated in adult fish, contrasting with mammals; the pre-set sequence of cell divisions in gametogenesis is otherwise similar and is described in detail. Most fish deposit much yolk (vitellogenesis) in developing eggs. Migrations, beach-spawning and mouth-brooding are some of the interesting variations. Fertilization is predominantly external but is internal in some groups such as chondrichthyans. The omission of annual reproduction is wel

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29

Rohling, Eelco J. The Climate Question. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190910877.001.0001.

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In 2015, annual average atmospheric carbon dioxide (CO2) levels surpassed a level of 400 parts per million (ppm) for the first time in three million years. This has caused widespread concern among climate scientists, and not least among those that work on natural climate variability in prehistoric times, before humans. These people are known as "past climate" or palaeoclimate researchers, and author Eelco J. Rohling is one of them. The Climate Question offers a background to these concerns in straightforward terms, with examples, and is motivated by Rohling's personal experience in being inten

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30

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can hav

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31

Szewczyk, Janusz. Rola zaburzeń w kształtowaniu struktury i dynamiki naturalnych lasów bukowo-jodłowo-świerkowych w Karpatach Zachodnich. Publishing House of the University of Agriculture in Krakow, 2018. http://dx.doi.org/10.15576/978-83-66602-35-9.

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The aim of the study was to determine the influence of different disturbances (both natural and anthropogenic) on species composition and stand structure of old-growth mixed mountain forests in the Western Carpathians. These stands are usually dominated by beech, fir and spruce, mixed in different proportions. The tree main species represent different growth strategies, and they compete against each other. The longevity of trees makes the factors influencing the stand structure difficult to identify, even during longitudinal studies conducted on permanent research plots. That is why dendroecol

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