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Articoli di riviste sul tema "Climatic changes"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 25 luglio 2025

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1

Kovács-Láng, E., Gy Kröel-Dulay, M. Kertész, et al. "Changes in the composition of sand grasslands along a climatic gradient in Hungary and implications for climate change." Phytocoenologia 30, no. 3-4 (2000): 385–407. http://dx.doi.org/10.1127/phyto/30/2000/385.

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2

ERONEN, MATTI. "Global climatic changes." Boreas 11, no. 1 (2008): 58. http://dx.doi.org/10.1111/j.1502-3885.1982.tb00521.x.

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3

Oriangi, George, Yazidhi Bamutaze, Paul Isolo Mukwaya, and Edekebon Elaijah. "Medium Term Climate Change Effects on Millet Yields in Gulu District, Northern Uganda." African Journal of Climate Change and Resource Sustainability 3, no. 1 (2024): 150–64. http://dx.doi.org/10.37284/ajccrs.3.1.1919.

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Climate change is expected to adversely affect crop yields and livelihoods of agro-dependent societies, especially in Sub-Saharan Africa. However, there remain gaps on the effects of expected regional climatic changes on key food security crops. This study assessed the projected climatic conditions and expected changes in millet yields for Paicho Sub County (S/C) in Gulu District up to the year 2033 using a cross sectional study design. To determine future climatic conditions, PRECIS (Providing Regional Climates for Impact Studies) model was used based on projected conditions at a 50 km spatia

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4

Stauffer, B., H. Oeschger, and J. Schwander. "Changes Of Atmospheric Methane Concentration Parallel To Climatic Changes." Annals of Glaciology 14 (1990): 359. http://dx.doi.org/10.3189/s0260305500009368.

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Measurements on ice-core samples showed that atmospheric methane concentration changed with the large climatic cycles during the last two glaciations (Stauffer and others, 1988; Raynaud and others, 1988). The methane concentration is lower in cold periods and higher in warm periods. In this paper we discuss the results of CH4 measurements of samples from periods of minor climatic change, like the climatic optimum 8000 years B.P. and the Younger Dryas period about 10 000 to 11 000 years B.P.. The data are interpreted in terms of the present understanding of methane sources and sinks.

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5

Stauffer, B., H. Oeschger, and J. Schwander. "Changes Of Atmospheric Methane Concentration Parallel To Climatic Changes." Annals of Glaciology 14 (1990): 359. http://dx.doi.org/10.1017/s0260305500009368.

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Measurements on ice-core samples showed that atmospheric methane concentration changed with the large climatic cycles during the last two glaciations (Stauffer and others, 1988; Raynaud and others, 1988). The methane concentration is lower in cold periods and higher in warm periods. In this paper we discuss the results of CH4 measurements of samples from periods of minor climatic change, like the climatic optimum 8000 years B.P. and the Younger Dryas period about 10 000 to 11 000 years B.P.. The data are interpreted in terms of the present understanding of methane sources and sinks.

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6

Radadiya, Sanjay. "Global Climatic Changes & its Effect on Agriculture." Indian Journal of Applied Research 2, no. 3 (2011): 120–22. http://dx.doi.org/10.15373/2249555x/dec2012/37.

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7

Mohammad Reza, Khaleghi. "Application of dendroclimatology in evaluation of climatic changes." Journal of Forest Science 64, No. 3 (2018): 139–47. http://dx.doi.org/10.17221/79/2017-jfs.

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The present study tends to describe the survey of climatic changes in the case of the Bojnourd region of North Khorasan, Iran. Climate change due to a fragile ecosystem in semi-arid and arid regions such as Iran is one of the most challenging climatological and hydrological problems. Dendrochronology, which uses tree rings to their exact year of formation to analyse temporal and spatial patterns of processes in the physical and cultural sciences, can be used to evaluate the effects of climate change. In this study, the effects of climate change were simulated using dendrochronology (tree rings

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8

Alvi, Shamsul Haque. "Climatic changes in Bahrain." GeoJournal 37, no. 1 (1995): 45–50. http://dx.doi.org/10.1007/bf00814884.

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9

Oriangi, George, Paul Isolo Mukwaya, Justine Kilama Luwa, Menya Emmanuel, Malinga Geoffrey Maxwell, and Yazidhi Bamutaze. "Variability and Changes in Climate in Northern Uganda." African Journal of Climate Change and Resource Sustainability 3, no. 1 (2024): 81–97. http://dx.doi.org/10.37284/ajccrs.3.1.1830.

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Variability and changes in climate are generally expected to occur. However, there remain gaps on dynamics of expected regional variations in climatic changes. This study assessed historic and projected climatic conditions up to the year 2033. The study hypothesized that temperature rather than rainfall significantly increased for the period 1980-2010 and rainfall rather than temperature is likely to decrease significantly by 2033 for Gulu District in northern Uganda. To determine historic climatic trends, rainfall and temperature data were obtained from Uganda National Meteorological Authorit

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10

KAUR, PRABHJYOT, NAVNEET KAUR, and HARPREET SINGH. "PRECIS-model simulated changes in climatic parameters under various scenarios in different agro-climatic zones of Punjab." MAUSAM 68, no. 1 (2021): 139–48. http://dx.doi.org/10.54302/mausam.v68i1.443.

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In this study,the future simulated climatic data (temperature and rainfall) for the 21st century were downscaled using the regional climate model, viz., PRECIS model (Providing Regional Climates for Impact Studies) for different agro-climatic zones, i.e., Zone II (Ballowal Saunkhri), Zone III (Ludhiana, Amritsar, Patiala and Jalandhar) and Zone V (Bathinda) of Punjab. The corrected simulated data were then analyzed on the annual and seasonal basis to quantify the changes in maximum and minimum temperature and rainfall. The study showed that the maximum and minimum temperature and rainfall by t

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11

Karataş, Kader Semra, and Sevda Ocak. "Climatic Changes and Psychiatric Disorders." Van Medical Journal 25, no. 2 (2018): 268–73. http://dx.doi.org/10.5505/vtd.2018.50455.

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12

Lécuyer, Christophe. "Learning from past climatic changes." Science 360, no. 6396 (2018): 1400–1401. http://dx.doi.org/10.1126/science.aau1690.

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13

Rosqvist, Gunhild. "Riukojietna’s Sensitivity To Climatic Changes." Annals of Glaciology 14 (1990): 357. http://dx.doi.org/10.3189/s0260305500009332.

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Riukojietna (lat. 68°N., long. 18°E.), which is classified as an ice cap, is located 35 km north-west of Kebnekaise, northern Sweden. The glacier is situated between 1140 and 1456 m a.s.l. and covers an area of 4.6 km2. The surrounding mountains reach the 1600 m level. Two maps, based on air photographs taken 1960 and 1978, have been produced. A study of sediments from two lakes receiving meltwater from Riukojietna has yielded information on Riukojietna’s ability to produce rock flour during the Holocene. Several factors affect the production and removal of rock flour of which the most importa

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14

Rosqvist, Gunhild. "Riukojietna’s Sensitivity To Climatic Changes." Annals of Glaciology 14 (1990): 357. http://dx.doi.org/10.1017/s0260305500009332.

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Abstract (sommario):

Riukojietna (lat. 68°N., long. 18°E.), which is classified as an ice cap, is located 35 km north-west of Kebnekaise, northern Sweden. The glacier is situated between 1140 and 1456 m a.s.l. and covers an area of 4.6 km2. The surrounding mountains reach the 1600 m level. Two maps, based on air photographs taken 1960 and 1978, have been produced. A study of sediments from two lakes receiving meltwater from Riukojietna has yielded information on Riukojietna’s ability to produce rock flour during the Holocene. Several factors affect the production and removal of rock flour of which the most importa

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15

O�ate Rubalcaba, Juan J., and Antonio Pou Royo. "Climatic changes in western Spain." International Journal of Biometeorology 39, no. 1 (1995): 22–28. http://dx.doi.org/10.1007/bf01320889.

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16

Prosperi, S. "Climatic Changes and Emerging Diseases." Veterinary Research Communications 30, S1 (2006): 83–86. http://dx.doi.org/10.1007/s11259-006-0017-9.

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17

Radwan, Eman, khaled Rradwan, Mohie Eldin Saber, Mennatallah Saber, and Ensaf Elgayar. "Impacts of the Climatic Changes." Journal of Desert and Environmental Agriculture 3, no. 1 (2023): 18–40. http://dx.doi.org/10.21608/jdea.2023.190362.1015.

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18

Crisan, Vlad, Lucian Dinca, Sorin Deca, Gruita Ienasoiu, and Virgil Scarlatescu. "SESSILE OAK FOREST ECOSYSTEMS FROM TRANSYLVANIA IN THE CONTEXT OF CLIMATIC CHANGES." Current Trends in Natural Sciences 10, no. 19 (2021): 48–57. http://dx.doi.org/10.47068/ctns.2021.v10i19.006.

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Climatic modelling software was used in order to measure future changes in climatic conditions. The software HYPE can realize prognosis for certain climatic factors responsible for causing extreme climatic phenomena in forest ecosystems. It was applied to study sessile oak forest ecosystems from Transylvania. Sample surfaces were installed, inventoried and followed by simulations of two future climatic scenarios. Two such scenarios were chosen, namely the climatic scenario in which the gas effect concentration will increase moderately (rcp-4.5) and the climatic scenario in which the gas effect

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19

Palmer, Georgina, Philip J. Platts, Tom Brereton, et al. "Climate change, climatic variation and extreme biological responses." Philosophical Transactions of the Royal Society B: Biological Sciences 372, no. 1723 (2017): 20160144. http://dx.doi.org/10.1098/rstb.2016.0144.

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Extreme climatic events could be major drivers of biodiversity change, but it is unclear whether extreme biological changes are (i) individualistic (species- or group-specific), (ii) commonly associated with unusual climatic events and/or (iii) important determinants of long-term population trends. Using population time series for 238 widespread species (207 Lepidoptera and 31 birds) in England since 1968, we found that population ‘crashes’ (outliers in terms of species' year-to-year population changes) were 46% more frequent than population ‘explosions’. (i) Every year, at least three species

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20

Crisan, Vlad, Lucian Dinca, Iuliana Gabriela Breaban, and Sorin Deca. "Analysing pine forest ecosystems from Transylvania in the context of future Climatic Changes." Present Environment and Sustainable Development 15, no. 2 (2021): 199–208. http://dx.doi.org/10.15551/pesd2021152016.

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A climatic modelling program was used in order to see the extent of changes in future climatic conditions. This can realize prognosis for certain climatic factors that cause extreme climatic phenomena concerning forest ecosystems. The program was applied for forest ecosystems comprised of Scots pine, installed and inventoried on sample surfaces from Transylvania. Simulations were then created within two future climatic scenarios. Two scenarios were chosen: the climatic scenario in which the increase of greenhouse gases would be moderate (rcp-4.5) and the climatic scenario in which the increase

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21

Zhang, Hucai, Bernd Wünnemann, Yuzhen Ma, et al. "Lake Level and Climate Changes between 42,000 and 18,000 14C yr B.P. in the Tengger Desert, Northwestern China." Quaternary Research 58, no. 1 (2002): 62–72. http://dx.doi.org/10.1006/qres.2002.2357.

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AbstractMultiple lines of stratigraphic, geochemical, and fossil data suggest that fresh-mesohaline paleolakes were widespread in the Tengger Desert of northwestern China and underwent major fluctuations during the late Pleistocene. The paleolakes started to develop at ca. 42,000 14C yr B.P. The lake levels were the highest between 35,000 and 22,000 14C yr B.P., during which Megalake Tengger dominated the landscape. The climatic conditions at this time were unique for this area and have no modern analogue. After an episode of decline between 22,000 and 20,000 14C yr B.P. and an episode of rebo

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22

Bell, Jason L., Lisa C. Sloan, and Mark A. Snyder. "Regional Changes in Extreme Climatic Events: A Future Climate Scenario." Journal of Climate 17, no. 1 (2004): 81–87. http://dx.doi.org/10.1175/1520-0442(2004)017<0081:rciece>2.0.co;2.

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23

Wang, Hui, and Jian Hua Cheng. "Influences of Abnormal Climates on Engineering Characteristics of Expansive Soil." Applied Mechanics and Materials 170-173 (May 2012): 800–803. http://dx.doi.org/10.4028/www.scientific.net/amm.170-173.800.

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Expansive soil is a kind of high plastic clay which is more sensitive to changes of climatic and hydrogeologic conditions, and it has the character of swelling when watering and shrinking when drying out. Such repeated fluctuations from dry to wet induce irreversible deformation ,which will make the shear strength and internal friction of soil drop sharply and cause slope fracture. In recent years, abnormal climatic changes worldwide make foundation stability of expansive soil face severe test . Atmospheric influence depth can supply design basis for slope fracture of expansive soil. But in th

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24

Bryson, Reid A. "Civilization and Rapid Climatic Change." Environmental Conservation 15, no. 1 (1988): 7–15. http://dx.doi.org/10.1017/s037689290002840x.

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Research over the past century has shown that the rates and magnitudes of climatic change constitute a continuum. Changes have now been identified in the climatic record that range in duration from interannual through decades and centuries to the multi-millennial time-scale. Examples range from the drought years of the 1930 and 1970 decades to the ponderous comings and goings of the ice-ages. More recently it has become clear that some changes can be quite rapid. In recent decades great progress has been made in identifying the causes of climatic variation.The present understanding of the caus

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25

Pelto, M. S., S. M. Higgins, T. J. Hughes, and J. L. Fastook. "Modeling Mass-Balance Changes During a Glaciation Cycle." Annals of Glaciology 14 (1990): 238–41. http://dx.doi.org/10.3189/s0260305500008661.

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Identification of present-day climate setting and alpine glacier-balance gradients indicates that the balance gradient of alpine glaciers is primarily determined by climatic conditions. Determination of balance gradients for specific climatic settings on present-day ice sheets provides an analog for determining the mass balance on paleo and future ice sheets.

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26

Pelto, M. S., S. M. Higgins, T. J. Hughes, and J. L. Fastook. "Modeling Mass-Balance Changes During a Glaciation Cycle." Annals of Glaciology 14 (1990): 238–41. http://dx.doi.org/10.1017/s0260305500008661.

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Identification of present-day climate setting and alpine glacier-balance gradients indicates that the balance gradient of alpine glaciers is primarily determined by climatic conditions. Determination of balance gradients for specific climatic settings on present-day ice sheets provides an analog for determining the mass balance on paleo and future ice sheets.

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27

Mastrandrea, Michael D., and Stephen H. Schneider. "Integrated assessment of abrupt climatic changes." Climate Policy 1, no. 4 (2001): 433–49. http://dx.doi.org/10.3763/cpol.2001.0146.

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28

Chendev, Yury, Aleksandr Petin, and Anthony Lupo. "SOILS AS INDICATORS OF CLIMATIC CHANGES." GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY 5, no. 1 (2012): 4–17. http://dx.doi.org/10.24057/2071-9388-2012-5-1-4-17.

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29

PRAMANIK, S. K., and P. JAGANNATHAN. "Climatic changes in India – (III) pressure." MAUSAM 6, no. 2 (2021): 137–48. http://dx.doi.org/10.54302/mausam.v6i2.4432.

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30

Baker, Victor. "Hydrologic impact of Holocene climatic changes." Boreas 33, no. 3 (2004): 267. http://dx.doi.org/10.1080/03009480310001929.

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Mastrandrea, M. "Integrated assessment of abrupt climatic changes." Climate Policy 1, no. 4 (2001): 433–49. http://dx.doi.org/10.1016/s1469-3062(01)00038-9.

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32

Ammann, Brigitta. "Biotic responses to rapid climatic changes." Palaeogeography, Palaeoclimatology, Palaeoecology 159, no. 3-4 (2000): 191–201. http://dx.doi.org/10.1016/s0031-0182(00)00084-5.

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33

Nagy, Esther. "Climatic changes in the Hungarian Miocene." Review of Palaeobotany and Palynology 65, no. 1-4 (1990): 71–74. http://dx.doi.org/10.1016/0034-6667(90)90057-p.

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34

BAKER, VICTOR R. "Hydrologic impact of Holocene climatic changes." Boreas 33, no. 3 (2008): 267. http://dx.doi.org/10.1111/j.1502-3885.2004.tb01147.x.

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35

Leftus, Vojtěch, J. Tomlain, and V. Vítek. "Solar activity variations and climatic changes." Studia Geophysica et Geodaetica 30, no. 1 (1986): 93–110. http://dx.doi.org/10.1007/bf01630858.

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36

Dr., Surendra Singh Mourya. "The Maintaining biodiversity and climatic changes." International Educational Applied Research Journal 09, no. 04 (2025): 52–58. https://doi.org/10.5281/zenodo.15319784.

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Human beings are not only a part of our planet's ecosystems, but also, they are massively overusing them. This makes ecosystem protection, including biodiversity preservation, vital for humanity's future. The speed and scale of the threat are unprecedented in human history. The long arch of evolution has been confronted with such a high level of human impact, that we are now facing the sixth mass extinction event, 66 million years after the last one. This threat heightens the imperative for bold human intervention. Our paper identifies three strategies for such an intervention. First

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37

Chiesa, Giacomo. "Climatic potential maps of ventilative cooling techniques in Italian climates including resilience to climate changes." IOP Conference Series: Materials Science and Engineering 609 (October 23, 2019): 032039. http://dx.doi.org/10.1088/1757-899x/609/3/032039.

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38

Skrobala, V. M., V. V. Popovych, P. V. Bosak, and T. I. Shuplat. "Prediction of changes in the vegetation cover of Ukraine due to climate warming." Naukovyi Visnyk Natsionalnoho Hirnychoho Universytetu, no. 4 (August 30, 2022): 96–105. http://dx.doi.org/10.33271/nvngu/2022-4/096.

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Purpose. To study ecological regularities of the formation of vegetation cover in Ukraine depending on the climatic conditions and analyze its possible changes due to global warming. Methodology. The research methodology involves the following: differentiation of the climatic conditions and evaluation of the significance of climatic indices at the level of territorial units of a geobotanical zoning based on variance analysis; multiple ordering of the geographic locations in terms of climatic indices basing on the analysis of main components (Principle Component Analysis); development of a typo

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39

Ruget, F., J. C. Moreau, M. Ferrand, et al. "Describing the possible climate changes in France and some examples of their effects on main crops used in livestock systems." Advances in Science and Research 4, no. 1 (2010): 99–104. http://dx.doi.org/10.5194/asr-4-99-2010.

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Abstract. The effects of climate change on forage and crop production are an important question for the farmers and more largely for the food security in the world. Estimating the effect of climate change on agricultural production needs the use of two types of tools: a model to estimate changes in national or local climates and an other model using climatic data to estimate the effects on vegetation. In this paper, we will mainly present the effects of climate change on climatic features, the variability of criteria influencing crop production in various regions of France and some possible ef

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40

Kalaugher, P. G., and P. Grainger. "The influence of changes in sea level on coastal cliff instability in Devon." Geological Society, London, Engineering Geology Special Publications 7, no. 1 (1991): 361–67. http://dx.doi.org/10.1144/gsl.eng.1991.007.01.31.

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AbstractMajor variations in sea level have resulted from climatic changes during the Quaternary. In addition, beyond the maximum limit of glaciation, periglacial climates in southern Britain have produced Quaternary deposits which can affect the nature of coastal slopes and their response to marine erosion. Examples are given of cliffs in head (solifluction) deposits which overlie raised shore platforms in Devon. The present styles and distribution of coastal landslide hazards, recorded in recent surveys, are directly related to past Quaternary sea levels and climatic fluctuations. Future tren

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Selek, Bulent, I. Kaan Tuncok, and Zeliha Selek. "Changes in climate zones across Turkey." Journal of Water and Climate Change 9, no. 1 (2017): 178–95. http://dx.doi.org/10.2166/wcc.2017.121.

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Abstract Turkey lies in a critical region that is projected to be one of the most vulnerable to the impacts of climate change in the Mediterranean region. In this study, climatic zones of Turkey were classified with respect to their climatic and meteorological characteristics. The Thornthwaite precipitation efficiency index was used to identify aridity and humidity characteristics. The index values were mapped to determine climate zones and associated climate classes and to evaluate change in time and space. Two distinct periods (1950–1980 and 1981–2010) were used to assess climatic conditions

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42

McGee, David. "Glacial–Interglacial Precipitation Changes." Annual Review of Marine Science 12, no. 1 (2020): 525–57. http://dx.doi.org/10.1146/annurev-marine-010419-010859.

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Glacial–interglacial cycles have constituted a primary mode of climate variability over the last 2.6 million years of Earth's history. While glacial periods cannot be seen simply as a reverse analogue of future warming, they offer an opportunity to test our understanding of the response of precipitation patterns to a much wider range of conditions than we have been able to directly observe. This review explores key features of precipitation patterns associated with glacial climates, which include drying in large regions of the tropics and wetter conditions in substantial parts of the subtropic

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Wan, Yangtao, Han Han, Yao Mao, and Bao-Jie He. "Responses of Climatic Drought to Vegetation Cover Dynamics: A Case Study in Yunnan, China." Forests 15, no. 10 (2024): 1689. http://dx.doi.org/10.3390/f15101689.

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Vegetation cover can regulate regional climate and associated dry–wet variations. However, the effects of the quantitative structure and landscape pattern of vegetation cover on climatic drought remain unclear. Yunnan Province in China, with its abundant vegetation resources, provides a good setting for addressing this research gap. Our objective is to provide guiding recommendations for climate-warming mitigation through the study of the topic. This study adopted four periods of vegetation cover data, from 1992 to 2020, and explored their dynamics. Monthly average precipitation and temperatur

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Dermody, B. J., H. J. de Boer, M. F. P. Bierkens, S. L. Weber, M. J. Wassen, and S. C. Dekker. "A seesaw in Mediterranean precipitation during the Roman Period linked to millennial-scale changes in the North Atlantic." Climate of the Past 8, no. 2 (2012): 637–51. http://dx.doi.org/10.5194/cp-8-637-2012.

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Abstract. We present a reconstruction of the change in climatic humidity around the Mediterranean between 3000–1000 yr BP. Using a range of proxy archives and model simulations we demonstrate that climate during this period was typified by a millennial-scale seesaw in climatic humidity between Spain and Israel on one side and the Central Mediterranean and Turkey on the other, similar to precipitation anomalies associated with the East Atlantic/West Russia pattern in current climate. We find that changes in the position and intensity of the jet stream indicated by our analysis correlate with mi

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45

Feng, Zhaodong, Aizhi Sun, Nurbayev Abdusalih, et al. "Vegetation changes and associated climatic changes in the southern Altai Mountains within China during the Holocene." Holocene 27, no. 5 (2016): 683–93. http://dx.doi.org/10.1177/0959683616670469.

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The location of the Altai Mountains at the limits of both the Pacific and Atlantic influences implies that this mountain range is an important climatic boundary. Based on pollen data of 188 samples of a 390-cm core from Narenxia Peat in the southern Altai with a chronologic support of 11 accelerator mass spectrometry (AMS) dates, we reconstructed the Holocene climatic change at Narenxia Peat. The reconstruction revealed five stages of climatic change: a cold and dry latest deglacial (prior to ~11,500 cal. yr BP), a warm and wet early-Holocene (~11,500 to ~7000 cal. yr BP), a considerably coole

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Ajjur, Salah Basem, and Emanuele Di Lorenzo. "Sensitivity of Groundwater Recharge Assessment to Input Data in Arid Areas." Hydrology 11, no. 2 (2024): 28. http://dx.doi.org/10.3390/hydrology11020028.

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Natural groundwater recharge (GR) assessment depends on several hydrogeological and climatic inputs, where uncertainty is inevitable. Assessing how inputs’ uncertainty affects GR estimation is important; however, it remains unclear in arid areas. This study assesses inputs’ uncertainty by examining the changes in GR simulations resulting from modifications in climatic, land use, and soil inputs. A physical-based hydrological model was built to estimate GR from 18 different GR scenarios across Qatar. Scenarios S1–S7 were created from different climatic inputs but identical land use and soil map

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Magny, Michel. "Paleohydrological Changes in Jura (France), and Climatic Oscillations around the North Atlantic from Allerød to Preboreal." Géographie physique et Quaternaire 49, no. 3 (2007): 401–8. http://dx.doi.org/10.7202/033062ar.

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ABSTRACTRegional palaeohydroiogical changes recorded in the Jura lakes, France, have led to a tentative reconstruction of a fine-scale pattern of climatic changes from Allerød to the early Holocene. The Younger Dryas (YD) can be subdivided into three parts: after a first wet phase, this cool period was characterized by increasing dryness; a short rise in lake level developed during its last part. Moreover, the YD was preceded and followed by two short rises in lake-level, which interrupted the lake-level lowerings developing during the Allerød and the Preboreal. Climatic oscillations reconstru

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48

Arkhipov, S. A., V. S. Volkova, V. A. Bakhareva, et al. "NATURAL CLIMATIC CHANGES IN WEST SIBERIA TO A.D. 2000." Russian Geology and Geophysics 35, no. 1 (1994): 1–16. https://doi.org/10.2113/rgg.1994.35.1.1.

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A prediction scenario of landscape-climatic setting to A.D. 2000 is proposed. It is based on the principle of paleoclimatic analogies, according to which the concentration of carbon dioxide in the atmosphere and in the ocean surface layer is correlated with the Earth’s global temperatures (Budyko, 1984; Zubakov, 1986, 1990). It is known that at the expense of anthropogenic factor the carbon dioxide concentration will be increased in A.D. 2000 to the values that existed during the Holocene climatic optimum. In this connection the landscape-climatic setting of this optimum, which fell on the per

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Iona, Athanasia, Athanasios Theodorou, Sarantis Sofianos, Sylvain Watelet, Charles Troupin, and Jean-Marie Beckers. "Mediterranean Sea climatic indices: monitoring long-term variability and climate changes." Earth System Science Data 10, no. 4 (2018): 1829–42. http://dx.doi.org/10.5194/essd-10-1829-2018.

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Abstract. We present a new product composed of a set of thermohaline climatic indices from 1950 to 2015 for the Mediterranean Sea such as decadal temperature and salinity anomalies, their mean values over selected depths, decadal ocean heat and salt content anomalies at selected depth layers as well as their long time series. It is produced from a new high-resolution climatology of temperature and salinity on a 1∕8∘ regular grid based on historical high-quality in situ observations. Ocean heat and salt content differences between 1980–2015 and 1950–1979 are compared for evaluation of the clima

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Ng, Edward, and Chao Ren. "China's adaptation to climate & urban climatic changes: A critical review." Urban Climate 23 (March 2018): 352–72. http://dx.doi.org/10.1016/j.uclim.2017.07.006.

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