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Journal articles on the topic 'Eurasian climate'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Feng, Jiajun, Yuanzhi Zhang, Jin Yeu Tsou, and Kapo Wong. "Analyzing Variations in the Association of Eurasian Winter–Spring Snow Water Equivalent and Autumn Arctic Sea Ice." Remote Sensing 14, no. 2 (2022): 243. http://dx.doi.org/10.3390/rs14020243.

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Because Eurasian snow water equivalent (SWE) is a key factor affecting the climate in the Northern Hemisphere, understanding the distribution characteristics of Eurasian SWE is important. Through empirical orthogonal function (EOF) analysis, we found that the first and second modes of Eurasian winter SWE present the distribution characteristics of an east–west dipole and north–south dipole, respectively. Moreover, the distribution of the second mode is caused by autumn Arctic sea ice, with the distribution of the north–south dipole continuing into spring. As the sea ice of the Barents–Kara Sea

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2

Khan, V. M. "Overview of current and expected seasonal climatic anomalies for the winter 2021/2022 with their possible impact on the economy, as estimated by the meteorological services of the CIS countries." Hydrometeorological research and forecasting 4 (December 16, 2021): 163–76. http://dx.doi.org/10.37162/2618-9631-2021-4-163-176.

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Based on assessments of the meteorological services of the CIS countries, the skill scores of the consensus forecast for the territory of Northern Eurasia for the summer of 2021 are presented. The results of monitoring circulation patterns in the stratosphere and troposphere over the past summer season are discussed. Climate monitoring and seasonal forecasting results for the current situation are presented. A probabilistic consensus forecast for air temperature and precipitation is presented for the upcoming winter season 2021/2022 in Northern Eurasia. Possible consequences of the impact of t

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3

Khan, V. M., R. M. Vilfand, E. V. Emelina, et al. "Climatic features of the 2020/2021 winter season and the air temperature and precipitation outlook for the summer of 2021 over Northern Eurasia." Hydrometeorological research and forecasting 2 (June 23, 2021): 6–19. http://dx.doi.org/10.37162/2618-9631-2021-2-6-19.

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Climatic features of the 2020/2021 winter season and the air temperature and precipitation outlook for the summer of 2021 over Northern Eurasia / Khan V.M., Vilfand R.M., Emelina E.V., Kaverina E.S., Kulikova I.A., Sumerova K.A., Tischenko V.A. // Hydrometeorological Research and Forecasting, 2021, no. 2 (380), pp. 6-19. The main features of the Northern Hemisphere large-scale atmospheric circulation are analyzed for the past 2020/2021 winter. The accuracy of consensus forecasts of air temperature and precipitation compiled during the work of the 19th session of the North Eurasian Climate Outl

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4

Khan, V. M., R. M. Vilfand, V. A. Tishchenko, et al. "Outcomes of 25th session of the North Eurasian Climate Outlook Forum combined with the project inception regional workshop under the auspices of the UN ESCAP: Enhancing knowledge and capacity to build resilience to slow-onset disasters in Central Asia / Khan V.M., Vilfand R.M., Tishchenko V.A., Sumerova K.A., Emelina S.V., Nabokova E.V., Kaverina E.S.,. Kulikova I.A, Kruglova E.N., Tolstykh M.A. // Hydrometeorological Research and Forecasting, 2023, no. 4 (390), pp. 154-169." Hydrometeorological research and forecasting 4 (December 15, 2023): 154–69. http://dx.doi.org/10.37162/2618-9631-2023-4-154-169.

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The North Eurasian Climate Center held the 25th session of the North Eurasian Climate Outlook Forum (NEACOF-25) combined with the project inception regional workshop under the auspices of the UN Economic and Social Commission for Asia and the Pacific (ESCAP). In total, 143 participants from 12 countries were registered at the event, 60 of them took part in the forum in person. During NEACOF-25, a consensus forecast of air temperature and precipitation anomalies for the territory of Northern Eurasia for the winter of 2023/2024 was presented. The NEACOF-25 consensus forecast is in agreement with

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Khan, V. M., R. M. Vilfand, V. A. Tishchenko, et al. "Outcomes of 25th session of the North Eurasian Climate Outlook Forum combined with the project inception regional workshop under the auspices of the UN ESCAP: Enhancing knowledge and capacity to build resilience to slow-onset disasters in Central Asia / Khan V.M., Vilfand R.M., Tishchenko V.A., Sumerova K.A., Emelina S.V., Nabokova E.V., Kaverina E.S.,. Kulikova I.A, Kruglova E.N., Tolstykh M.A. // Hydrometeorological Research and Forecasting, 2023, no. 4 (390), pp. 154-169." Hydrometeorological research and forecasting 4 (December 15, 2023): 154–69. http://dx.doi.org/10.37162/2618-9631-2023-4-154-169.

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The North Eurasian Climate Center held the 25th session of the North Eurasian Climate Outlook Forum (NEACOF-25) combined with the project inception regional workshop under the auspices of the UN Economic and Social Commission for Asia and the Pacific (ESCAP). In total, 143 participants from 12 countries were registered at the event, 60 of them took part in the forum in person. During NEACOF-25, a consensus forecast of air temperature and precipitation anomalies for the territory of Northern Eurasia for the winter of 2023/2024 was presented. The NEACOF-25 consensus forecast is in agreement with

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6

Liakka, Johan, Marcus Löfverström, and Florence Colleoni. "The impact of the North American glacial topography on the evolution of the Eurasian ice sheet over the last glacial cycle." Climate of the Past 12, no. 5 (2016): 1225–41. http://dx.doi.org/10.5194/cp-12-1225-2016.

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Abstract. Modeling studies have shown that the continental-scale ice sheets in North America and Eurasia in the last glacial cycle had a large influence on the atmospheric circulation and thus yielded a climate distinctly different from the present. However, to what extent the two ice sheets influenced each others' growth trajectories remains largely unexplored. In this study we investigate how an ice sheet in North America influences the downstream evolution of the Eurasian ice sheet, using a thermomechanical ice-sheet model forced by climate data from atmospheric snapshot experiments of thre

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7

Khan, V. M. "Outcomes of the 27th session of the North Eurasian Climate Outlook Forum combined with the UN ESCAP workshop." Hydrometeorological research and forecasting 4 (December 20, 2024): 163–78. https://doi.org/10.37162/2618-9631-2024-4-163-178.

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The North Eurasian Climate Centre held the 27th session of the North Eurasian Climate Outlook Forum (NEACOF-27) combined with a workshop under the auspices of the United Nations Economic and Social Commission for Asia and the Pacific (ESCAP), as a parallel section within the 8th All-Russian Joint Meteorological and Hydrological Congress. The joint event served as an important platform for the exchange of knowledge and experience in the field of climate research, seasonal forecasting and adaptation to climate change, which emphasized its importance for regional cooperation. During the forum, a

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8

Xu, Xinping, Shengping He, Botao Zhou, and Bo Sun. "CMIP6 near-term and long-term projections of Eurasian winter cooling trend and cold extremes." Environmental Research Letters 19, no. 10 (2024): 104038. http://dx.doi.org/10.1088/1748-9326/ad7307.

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Abstract It is well-known that climate warming increases air temperature and reduces cold extremes in the long-term. But internal variability strongly modulates the variability of temperature at mid- and- high latitudes, for example, causing the remarkable cooling and severe winter weather over Eurasia from the 1990s to the early 2010s. It remains unclear whether the occurrence of Eurasian cooling and cold extremes will be offset by climate warming or stimulated by internal variability in the future. Based on the Sixth phase of the Coupled Model Intercomparison Project multi-model projections

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9

Graham, Jim, Catherine Jarnevich, Nick Young, Greg Newman, and Thomas Stohlgren. "How will climate change affect the potential distribution of Eurasian tree sparrows Passer montanus in North America?" Current Zoology 57, no. 5 (2011): 648–54. http://dx.doi.org/10.1093/czoolo/57.5.648.

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Abstract Habitat suitability models have been used to predict the present and future potential distribution of a variety of species. Eurasian tree sparrows Passer montanus, native to Eurasia, have established populations in other parts of the world. In North America, their current distribution is limited to a relatively small region around its original introduction to St. Louis, Missouri. We combined data from the Global Biodiversity Information Facility with current and future climate data to create habitat suitability models using Maxent for this species. Under projected climate change scena

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10

Liu, Y., and J. C. H. Chiang. "Coordinated Abrupt Weakening of the Eurasian and North African Monsoons in the 1960s and Links to Extratropical North Atlantic Cooling." Journal of Climate 25, no. 10 (2012): 3532–48. http://dx.doi.org/10.1175/jcli-d-11-00219.1.

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Abstract Previous modeling and paleoclimate studies have suggested that cooling originating from the extratropical North Atlantic can abruptly weaken the Eurasian and North African monsoons. The climatic signature includes a widespread cooling over the Eurasian and North African continents and an associated increase to surface pressure. It is explored whether such coordinated changes are similarly exhibited in the observed twentieth-century climate, in particular with the well-documented shift of Sahel rainfall during the 1960s. Surface temperature, sea level pressure, and precipitation change

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Shinoda, Masato, Troy Sternberg, and Banzragch Nandintsetseg. "Multiple climate hazards in Eurasian drylands." Natural Hazards 92, S1 (2018): 1–2. http://dx.doi.org/10.1007/s11069-018-3516-4.

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12

Khan, V. M., R. M. Vilfand, S. V. Emelina, et al. "Twenty-second session of North Eurasian Climate Outlook Forum (NEACOF-22)." Hydrometeorological research and forecasting 2 (June 16, 2022): 181–84. http://dx.doi.org/10.37162/2618-9631-2022-2-181-184.

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The main results of the 22th session of the North Eurasian Climate Forum (NEACOF-22) in videoconference mode on May 26, 2022 are presented. Specialists from the research institutes and forecast organizations of Roshydromet, experts from meteorological services and research centers of the CIS countries, as well as scientists, teachers, graduate students and students of higher educational institutions with a specialization in meteorology and climatology, and other interested persons took part in NEACOF-22. In total, 112 participants from 9 countries were registered. Keywords: North Eurasian Clim

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13

Flanner, M. G., C. S. Zender, P. G. Hess, et al. "Springtime warming and reduced snow cover from carbonaceous particles." Atmospheric Chemistry and Physics 9, no. 7 (2009): 2481–97. http://dx.doi.org/10.5194/acp-9-2481-2009.

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Abstract. Boreal spring climate is uniquely susceptible to solar warming mechanisms because it has expansive snow cover and receives relatively strong insolation. Carbonaceous particles can influence snow coverage by warming the atmosphere, reducing surface-incident solar energy (dimming), and reducing snow reflectance after deposition (darkening). We apply a range of models and observations to explore impacts of these processes on springtime climate, drawing several conclusions: 1) Nearly all atmospheric particles (those with visible-band single-scatter albedo less than 0.999), including all

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14

Fu, Aihua, Erhu Gao, Xiaoping Tang, et al. "MaxEnt Modeling for Predicting the Potential Wintering Distribution of Eurasian Spoonbill (Platalea leucorodia leucorodia) under Climate Change in China." Animals 13, no. 5 (2023): 856. http://dx.doi.org/10.3390/ani13050856.

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Global climate change has become a trend and is one of the main factors affecting biodiversity patterns and species distributions. Many wild animals adapt to the changing living environment caused by climate change by changing their habitats. Birds are highly sensitive to climate change. Understanding the suitable wintering habitat of the Eurasian Spoonbill (Platalea leucorodia leucorodia) and its response to future climatic change is essential for its protection. In China, it was listed as national grade II key protected wild animal in the adjusted State List of key protected wild animals in

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15

Lubkov, A. S., E. N. Voskresenskaya, and O. V. Marchukova. "Recent El-Nino classification and associated climate response comparisons for the Atlantic-Eurasian region." Monitoring systems of environment, no. 1 (March 22, 2017): 94–100. http://dx.doi.org/10.33075/2220-5861-2017-1-94-100.

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Comparative study of El Nino classification after different authors results and approaches. The preferences of objective spatio-temporal classification which done earlier by the authors of present paper were shown for climate manifestation study over the Atlanic-Eurasian region. Using of NCEP/NCAR reanalysis data on sea level pressure in 1948-2016 the El-Nino types manifestations were estimated in Azor high, Iceland low and Siberian anticyclone. On this basis, appropriate prognostic estimates of typical climate anomalies in the Atlantic-Eurasian region are made. Next, the previous predictions

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16

Matsumura, Shinji, and Koji Yamazaki. "Eurasian Subarctic Summer Climate in Response to Anomalous Snow Cover." Journal of Climate 25, no. 4 (2012): 1305–17. http://dx.doi.org/10.1175/2011jcli4116.1.

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Abstract The summer climate in northern Eurasia is examined as a function of anomalous snow cover and processes associated with land–atmosphere coupling, based on a composite analysis using observational and reanalysis data. The analysis confirms that the snow–hydrological effect, which is enhanced soil moisture persisting later into the summer and contributing to cooling and precipitation recycling, is active in eastern Siberia and contributes to the formation of the subpolar jet through the thermal wind relationship in early snowmelt years. Strong anticyclonic differences (early − late snowm

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17

Chen, Shangfeng, Renguang Wu, Wen Chen, and Shuailei Yao. "Enhanced Linkage between Eurasian Winter and Spring Dominant Modes of Atmospheric Interannual Variability since the Early 1990s." Journal of Climate 31, no. 9 (2018): 3575–95. http://dx.doi.org/10.1175/jcli-d-17-0525.1.

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The present study reveals a marked enhancement in the relationship between Eurasian winter and spring atmospheric interannual variability since the early 1990s. Specifically, the dominant mode of winter Eurasian 500-hPa geopotential height anomalies, with same-sign anomalies over southern Europe and East Asia and opposite-sign anomalies over north-central Eurasia, is largely maintained to the following spring after the early 1990s, but not before the early 1990s. The maintenance of the dominant atmospheric circulation anomaly pattern after the early 1990s is associated with a triple sea surfac

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18

Massoud, Elias C., Young-Kwon Lim, Lauren C. Andrews, and Manuela Girotto. "Connecting Global Modes of Variability to Climate in High Mountain Asia." Atmosphere 15, no. 2 (2024): 142. http://dx.doi.org/10.3390/atmos15020142.

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Oscillations in global modes of variability (MoVs) form global teleconnections that affect regional climate variability and modify the potential for severe and damaging weather conditions. Understanding the link between certain MoVs and regional climate can improve the ability to more accurately predict environmental conditions that impact human life and health. In this study, we explore the connection between different MoVs, including the Arctic oscillation (AO), Eurasian teleconnection, Indian Ocean dipole (IOD), North Atlantic oscillation (NAO), and El Niño southern oscillation (Nino34), wi

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19

Martin, Craig R., Oliver Jagoutz, Rajeev Upadhyay, et al. "Paleocene latitude of the Kohistan–Ladakh arc indicates multistage India–Eurasia collision." Proceedings of the National Academy of Sciences 117, no. 47 (2020): 29487–94. http://dx.doi.org/10.1073/pnas.2009039117.

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We report paleomagnetic data showing that an intraoceanic Trans-Tethyan subduction zone existed south of the Eurasian continent and north of the Indian subcontinent until at least Paleocene time. This system was active between 66 and 62 Ma at a paleolatitude of 8.1 ± 5.6 °N, placing it 600–2,300 km south of the contemporaneous Eurasian margin. The first ophiolite obductions onto the northern Indian margin also occurred at this time, demonstrating that collision was a multistage process involving at least two subduction systems. Collisional events began with collision of India and the Trans-Tet

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20

Chen, Longhu, Qinqin Wang, Guofeng Zhu, et al. "Dataset of stable isotopes of precipitation in the Eurasian continent." Earth System Science Data 16, no. 3 (2024): 1543–57. http://dx.doi.org/10.5194/essd-16-1543-2024.

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Abstract. Stable isotopes in precipitation can effectively reveal the process of atmospheric water circulation, serving as an effective tool for hydrological and water resource research, climate change, and ecosystem studies. The scarcity of stable isotope data in precipitation has hindered comprehension of the regional hydrology, climate, and ecology due to discontinuities on a temporal scale and unevenness on a spatial scale. To this end, we collated stable hydrogen and oxygen isotope data in precipitation from 842 stations in Eurasia from 1961 to 2022, totalling 51 752 data records. Stable

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Li, Xinyu, Riyu Lu, and Joong-Bae Ahn. "Combined Effects of the British–Baikal Corridor Pattern and the Silk Road Pattern on Eurasian Surface Air Temperatures in Summer." Journal of Climate 34, no. 9 (2021): 3707–20. http://dx.doi.org/10.1175/jcli-d-20-0325.1.

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AbstractThe summer British–Baikal Corridor pattern (BBC) and the Silk Road pattern (SRP) manifest as zonally oriented teleconnections in the high and middle latitudes, respectively, of the Eurasian continent. In this study, we investigate the combined effects of the BBC and SRP on surface air temperatures over the Eurasian continent. It is found that the combination of the BBC and SRP results in two kinds of well-organized, large-scale circulation anomalies: the zonal tripole pattern and the Ω-like pattern in the 200-hPa geopotential height anomalies. The zonal tripole pattern is characterized

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Beghin, P., S. Charbit, M. Kageyama, C. Dumas, and C. Ritz. "How might the North American ice sheet influence the Northwestern Eurasian climate?" Climate of the Past Discussions 11, no. 1 (2015): 27–61. http://dx.doi.org/10.5194/cpd-11-27-2015.

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Abstract. During the last glacial period (∼21 000 years ago), two continental-scale ice sheets covered the Canada and northern Europe. It is now widely acknowledged that these past ice sheets exerted a strong influence on climate by causing changes in atmospheric and oceanic circulations. In turn, these changes may have impacted the development of the ice sheets themselves through a combination of different feedback mechanisms. The present study is designed to investigate the potential impact of the North American ice sheet on the surface mass balance (SMB) of the Eurasian ice sheet through si

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23

Zhang, Peng, Bin Wang, and Zhiwei Wu. "Weak El Niño and Winter Climate in the Mid- to High Latitudes of Eurasia." Journal of Climate 32, no. 2 (2018): 405–21. http://dx.doi.org/10.1175/jcli-d-17-0583.1.

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Abstract According to the sea surface temperature anomaly (SSTA) intensity in the Niño-3.4 region and the east–west gradient across the Pacific, three types of El Niño are identified in this work. An event with larger than average intensity is defined as a strong El Niño, all others are considered to be weak events. Almost all strong El Niños are concurrent with a large gradient, which is featured by negative SSTAs in the western Pacific and positive SSTAs in the equatorial eastern Pacific (EP) and Indian Ocean (IO). According to the east–west gradient, the weak events can be subdivided into g

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Ye, Kunhui, Gabriele Messori, Deliang Chen, and Tim Woollings. "An NAO-dominated mode of atmospheric circulation drives large decadal changes in wintertime surface climate and snow mass over Eurasia." Environmental Research Letters 17, no. 4 (2022): 044025. http://dx.doi.org/10.1088/1748-9326/ac592f.

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Abstract The leading mode of wintertime atmospheric variability over the North Atlantic-North Eurasia sector is dominated by the North Atlantic Oscillation (NAO) and accounts for more than one third of the total variability. This study explores the influences of the leading mode on decadal climate variability of Northern Eurasia. We focus on the little-explored decadal covariations of surface air temperature (SAT), snowfall, snow water equivalent (SWE) and snow cover over the region, using extensive model output from the Coupled Model Intercomparison Project sixth phase. Recent decadal trends

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Polvani, Lorenzo M., Lantao Sun, Amy H. Butler, Jadwiga H. Richter, and Clara Deser. "Distinguishing Stratospheric Sudden Warmings from ENSO as Key Drivers of Wintertime Climate Variability over the North Atlantic and Eurasia." Journal of Climate 30, no. 6 (2017): 1959–69. http://dx.doi.org/10.1175/jcli-d-16-0277.1.

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Stratospheric conditions are increasingly being recognized as an important driver of North Atlantic and Eurasian climate variability. Mindful that the observational record is relatively short, and that internal climate variability can be large, the authors here analyze a new 10-member ensemble of integrations of a stratosphere-resolving, atmospheric general circulation model, forced with the observed evolution of sea surface temperature (SST) during 1952–2003. Previous studies are confirmed, showing that El Niño conditions enhance the frequency of occurrence of stratospheric sudden warmings (S

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Huang, Jinlong, and Wenshou Tian. "Eurasian Cold Air Outbreaks under Different Arctic Stratospheric Polar Vortex Strengths." Journal of the Atmospheric Sciences 76, no. 5 (2019): 1245–64. http://dx.doi.org/10.1175/jas-d-18-0285.1.

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Abstract This study analyzes the differences and similarities of Eurasian cold air outbreaks (CAOs) under the weak (CAOW), strong (CAOS), and neutral (CAON) stratospheric polar vortex states and examines the potential links between the polar vortex and Eurasian CAOs. The results indicate that the colder surface air temperature (SAT) over Europe in the earlier stages of CAOW events is likely because the amplitude of the preexisting negative North Atlantic Oscillation pattern is larger in CAOW events than in CAON and CAOS events. Marked by the considerably negative stratospheric Arctic Oscillati

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Liakka, J., M. Löfverström, and F. Colleoni. "The impact of the North American ice sheet on the evolution of the Eurasian ice sheet during the last glacial cycle." Climate of the Past Discussions 11, no. 6 (2015): 5203–41. http://dx.doi.org/10.5194/cpd-11-5203-2015.

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Abstract. Modeling studies show that the massive ice sheet expanding over the North American and Eurasian continents in the last glacial cycle has a large impact on the atmospheric stationary waves and thus yielded a glacial climate distinctly different from the present. However, to what extent the two ice sheets influenced each others growth trajectories remains largely unexplored. In this study we investigate how ice sheets in North America influence the downstream evolution of the Eurasian ice sheet, using a thermomechanical ice-sheet model forced by climate data from snapshot simulations o

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28

Usoltsev, Vladimir А., Agnieszka Piernik, Anna A. Osmirko, Ivan S. Tsepordey, Viktor P. Chasovskikh, and Walery Zukow. "Forest stand biomass of Picea spp.: an additive model that may be related to climate and civilisational changes." Bulletin of Geography. Socio-economic Series 45, no. 45 (2019): 133–47. http://dx.doi.org/10.2478/bog-2019-0029.

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AbstractSince ancient times, climate change has largely determined the fate of human civilisation, which was related mainly to changes in the structure and habitats of forest cover. In the context of current climate change, one must know the capabilities of forests to stabilise the climate by increasing biomass and carbon-depositing abilities. For this purpose, the authors compiled a database of harvest biomass (t/ha) in 900 spruce (Picea spp.) sample plots in the Eurasian area and used the methodology of multivariate regression analysis. The first attempt at modelling changes in the biomass a

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Zhang, Xuanze, Yongqiang Zhang, Ning Ma, et al. "Greening-induced increase in evapotranspiration over Eurasia offset by CO₂-induced vegetational stomatal closure." Environmental Research Letters 16, no. 12 (2021): 124008. http://dx.doi.org/10.1088/1748-9326/ac3532.

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Abstract Evapotranspiration (ET), as a key exchanging component of the land energy, water and carbon cycles, is expected to increase in response to greening land under a warming climate. However, the relative importance of major drivers (e.g. leaf area index (LAI), climate forcing, atmospheric CO2, etc) to long-term ET change remain largely unclear. Focusing on the Eurasia which experienced the strong vegetational greening, we aim to estimate the long-term ET trend and its drivers’ relative contributions by applying a remote sensing-based water-carbon coupling model— Penman–Monteith–Leuning ve

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Ponomarev, Vasiliy, Georgiy Klobukov, Viktoria Napalkova, et al. "Phenological Features of the Spongy Moth, Lymantria dispar (L.) (Lepidoptera: Erebidae), in the Northernmost Portions of Its Eurasian Range." Insects 14, no. 3 (2023): 276. http://dx.doi.org/10.3390/insects14030276.

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The spongy moth, Lymatria dispar, is a classic example of an invasive pest accidentally introduced from Europe to North America, where it has become one of the most serious forest defoliators, as in its native range. The present study was aimed at (i) identifying the current northern limit of L. dispar’s Eurasian range and exploring its northward expansion in Canada using pheromone trap data, and (ii) comparing northern Eurasian populations with those from central and southern regions with respect to male flight phenology, the sums of effective temperatures (SETs) above the 7 °C threshold nece

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Lofverstrom, Marcus, and Johan Liakka. "The influence of atmospheric grid resolution in a climate model-forced ice sheet simulation." Cryosphere 12, no. 4 (2018): 1499–510. http://dx.doi.org/10.5194/tc-12-1499-2018.

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Abstract. Coupled climate–ice sheet simulations have been growing in popularity in recent years. Experiments of this type are however challenging as ice sheets evolve over multi-millennial timescales, which is beyond the practical integration limit of most Earth system models. A common method to increase model throughput is to trade resolution for computational efficiency (compromise accuracy for speed). Here we analyze how the resolution of an atmospheric general circulation model (AGCM) influences the simulation quality in a stand-alone ice sheet model. Four identical AGCM simulations of the

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Beghin, P., S. Charbit, C. Dumas, M. Kageyama, and C. Ritz. "How might the North American ice sheet influence the northwestern Eurasian climate?" Climate of the Past 11, no. 10 (2015): 1467–90. http://dx.doi.org/10.5194/cp-11-1467-2015.

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Abstract. It is now widely acknowledged that past Northern Hemisphere ice sheets covering Canada and northern Europe at the Last Glacial Maximum (LGM) exerted a strong influence on climate by causing changes in atmospheric and oceanic circulations. In turn, these changes may have impacted the development of the ice sheets themselves through a combination of different feedback mechanisms. The present study is designed to investigate the potential impact of the North American ice sheet on the surface mass balance (SMB) of the Eurasian ice sheet driven by simulated changes in the past glacial atm

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Wegmann, Martin, Yvan Orsolini, Antje Weisheimer, Bart van den Hurk, and Gerrit Lohmann. "Impact of Eurasian autumn snow on the winter North Atlantic Oscillation in seasonal forecasts of the 20th century." Weather and Climate Dynamics 2, no. 4 (2021): 1245–61. http://dx.doi.org/10.5194/wcd-2-1245-2021.

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Abstract. As the leading climate mode of wintertime climate variability over Europe, the North Atlantic Oscillation (NAO) has been extensively studied over the last decades. Recently, studies highlighted the state of the Eurasian cryosphere as a possible predictor for the wintertime NAO. However, missing correlation between snow cover and wintertime NAO in climate model experiments and strong non-stationarity of this link in reanalysis data are questioning the causality of this relationship. Here we use the large ensemble of Atmospheric Seasonal Forecasts of the 20th Century (ASF-20C) with the

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Wegmann, Martin, Yvan Orsolini, Emanuel Dutra, Olga Bulygina, Alexander Sterin, and Stefan Brönnimann. "Eurasian snow depth in long-term climate reanalyses." Cryosphere 11, no. 2 (2017): 923–35. http://dx.doi.org/10.5194/tc-11-923-2017.

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Abstract. Snow cover variability has significant effects on local and global climate evolution. By changing surface energy fluxes and hydrological conditions, changes in snow cover can alter atmospheric circulation and lead to remote climate effects. To document such multi-scale climate effects, atmospheric reanalysis and derived products offer the opportunity to analyze snow variability in great detail far back to the early 20th century. So far only little is know about their quality. Comparing snow depth in four long-term reanalysis datasets with Russian in situ snow depth data, we find a mo

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Gao, Yongqi, Jianqi Sun, Fei Li, et al. "Arctic sea ice and Eurasian climate: A review." Advances in Atmospheric Sciences 32, no. 1 (2014): 92–114. http://dx.doi.org/10.1007/s00376-014-0009-6.

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Zhao, Jia-Qiang, Tai Gao, Jing-Jing Du, and Juan Shi. "Future Trends in Obolodiplosis robiniae Distribution across Eurasian Continent under Global Climate Change." Insects 14, no. 1 (2023): 48. http://dx.doi.org/10.3390/insects14010048.

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Obolodiplosis robiniae was discovered in Eurasia at the beginning of the 21st century. In this study, we explore the present and future (in the years 2050 and 2070) trends in the potential distribution of O. robiniae in Eurasia under diverse climate change scenarios based on a maximum entropy model. Our findings indicated that the current potential distribution area of O. robiniae is within the range of 21°34′ and 65°39′ N in the Eurasian continent. The primary factor controlling the distribution of O. robiniae is temperature. The highly and moderately suitable areas are mainly distributed in

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Yasunari, Tetsuzo, Akio Kitoh, and Tatsushi Tokioka. "Effect Of Eurasian Snow Cover On Summer Climate Of The Northern Hemisphere: A GCM Study." Annals of Glaciology 14 (1990): 364. http://dx.doi.org/10.3189/s0260305500009447.

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Observational studies have shown that Eurasian snow-cover anomalies during winter-through-spring seasons have a great effect on anomalies in atmospheric circulation and climate in the following summer season through snow albedo feedback (Hahn and Shukla, 1976; Dey and Bhanu Kumar, 1987). Morinaga and Yasunari (1987) have revealed that large-scale snow-cover extent over central Asia in late winter, which particularly has a great effect on the circulation over Eurasia in the following season, is closely related to the Eurasian pattern circulation (Wallace and Gutzler, 1981) in the beginning of w

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Yasunari, Tetsuzo, Akio Kitoh, and Tatsushi Tokioka. "Effect Of Eurasian Snow Cover On Summer Climate Of The Northern Hemisphere: A GCM Study." Annals of Glaciology 14 (1990): 364. http://dx.doi.org/10.1017/s0260305500009447.

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Observational studies have shown that Eurasian snow-cover anomalies during winter-through-spring seasons have a great effect on anomalies in atmospheric circulation and climate in the following summer season through snow albedo feedback (Hahn and Shukla, 1976; Dey and Bhanu Kumar, 1987). Morinaga and Yasunari (1987) have revealed that large-scale snow-cover extent over central Asia in late winter, which particularly has a great effect on the circulation over Eurasia in the following season, is closely related to the Eurasian pattern circulation (Wallace and Gutzler, 1981) in the beginning of w

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Kleinen, Thomas, Pavel Tarasov, Victor Brovkin, Andrei Andreev, and Martina Stebich. "Comparison of modeled and reconstructed changes in forest cover through the past 8000 years." Holocene 21, no. 5 (2011): 723–34. http://dx.doi.org/10.1177/0959683610386980.

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Reproducing the tree cover changes throughout the Holocene is a challenge for land surface–atmosphere models. Here, results of a transient Holocene simulation of the coupled climate–carbon cycle model, CLIMBER2-LPJ, driven by changes in orbital forcing, are compared with pollen data and pollen-based reconstructions for several regions of Eurasia in terms of changes in tree fraction. The decline in tree fraction in the high latitudes suggested by data and model simulations is driven by a decrease in summer temperature over the Holocene. The cooler and drier trend at the eastern side of the Eura

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Fedorov, Vadim B., Emiliano Trucchi, Anna V. Goropashnaya, Eric Waltari, Susan Erin Whidden, and Nils Chr Stenseth. "Impact of past climate warming on genomic diversity and demographic history of collared lemmings across the Eurasian Arctic." Proceedings of the National Academy of Sciences 117, no. 6 (2020): 3026–33. http://dx.doi.org/10.1073/pnas.1913596117.

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The Arctic climate was warmer than today at the last interglacial and the Holocene thermal optimum. To reveal the impact of past climate-warming events on the demographic history of an Arctic specialist, we examined both mitochondrial and nuclear genomic variation in the collared lemming (Dicrostonyx torquatus, Pallas), a keystone species in tundra communities, across its entire distribution in northern Eurasia. The ancestral phylogenetic position of the West Beringian group and divergence time estimates support the hypothesis of continental range contraction to a single refugial area located

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Ji, Liuqing, and Ke Fan. "Climate Prediction of Satellite-Based Spring Eurasian Vegetation Index (NDVI) using Coupled Singular Value Decomposition (SVD) Patterns." Remote Sensing 11, no. 18 (2019): 2123. http://dx.doi.org/10.3390/rs11182123.

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Satellite-based normalized difference vegetation index (NDVI) data are widely used for estimating vegetation greenness. Seasonal climate predictions of spring (April–May–June) NDVI over Eurasia are explored by applying the year-to-year increment approach. The prediction models were developed based on the coupled modes of singular value decomposition (SVD) analyses between Eurasian NDVI and climate factors. One synchronous predictor, the spring surface air temperature from the NCEP’s Climate Forecast System (SAT-CFS), and three previous-season predictors (winter (December–January–February) sea-

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Prince, Candice M., Gregory E. MacDonald, and John E. Erickson. "Effects of Elevated Temperature and Carbon Dioxide Concentrations on the Response of Two Common Reed (Phragmites australis) Haplotypes to Glyphosate." Invasive Plant Science and Management 11, no. 4 (2018): 181–90. http://dx.doi.org/10.1017/inp.2018.25.

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AbstractCommon reed [Phragmites australis (Cav.) Trin. ex Steud.], an aggressive invader in North American wetlands, is likely to undergo a range expansion as the climate changes. Increased atmospheric [CO2] and temperature have been shown to cause morphological and physiological changes in many species, sometimes altering the way they respond to herbicides. To understand how climate-related environmental parameters may impact P. australis management, we grew two P. australis haplotypes (the Gulf Coast type and the Eurasian type) under ambient (400 ppm CO2, 32/21 C) or elevated (650 ppm CO2, 3

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BECKER, B. D., J. M. SLINGO, L. FERRANTI, and F. MOLTENI. "Seasonal predictability of the Indian Summer Monsoon : What role do land surface conditions play?" MAUSAM 52, no. 1 (2021): 175–90. http://dx.doi.org/10.54302/mausam.v52i1.1686.

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Anomalous springtime snow amounts over Eurasia may provide long term memory to the climate system by affecting the land surface energy and moisture budgets. In turn the anomalous land surface conditions introduced by snow anomalies may influence monsoon variability. In this paper, results from a programme of seasonal forecast ensembles are used to address, specifically, the influence of western Eurasian land surface conditions on the variability and hence predictability of the Indian summer monsoon. The factors that are important for establishing spring time land surface conditions over wester

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Jokimäki, Jukka, Marja-Liisa Kaisanlahti-Jokimäki, and Jukka Suhonen. "Long-Term Winter Population Trends of Corvids in Relation to Urbanization and Climate at Northern Latitudes." Animals 12, no. 14 (2022): 1820. http://dx.doi.org/10.3390/ani12141820.

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Corvids (crows, magpies, jays) live in a close association with humans, and therefore knowledge about their population status and changes will be an essential part of monitoring the quality of urban environments. Wintering bird populations can track habitat and climate changes more rapidly than breeding populations. We conducted a long-term (1991–2020) winter census of corvid species in 31 human settlements along a 920 km latitudinal gradient in Finland. We observed a total of five corvid species: the Eurasian Magpie (occurring in 114 surveys out of 122; total abundance 990 ind.), the Hooded C

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Subetto, A. I., and V. A. Shamakhov. "Russia — a Eurasian Civilization." EURASIAN INTEGRATION: economics, law, politics 14, no. 2 (2021): 26–39. http://dx.doi.org/10.22394/2073-2929-2021-02-26-39.

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The article argues that Russia as a “Eurasian civilization”, precisely as a “Eurasian” one, is the only civilization in the world. In the process of civilizational-Eurasian genesis, the historical synthesis of the “Western” (European) and “Eastern” (Asian) principles, expressed in its special value genome, is performed in it. Due to the “cold” climate in the Eurasian territory occupied by Russia, it is the highest energy-cost civilization and, therefore, — a civilization with the dominant role of the cooperation law. The Russian people, due to the peculiarity of their value aspirations, which

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Webster, P. "CLIMATE CHANGE: A Eurasian Tiger Threatens to Maul Kyoto." Science 303, no. 5663 (2004): 1461–62. http://dx.doi.org/10.1126/science.303.5663.1461.

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Cohen, Judah, and Dara Entekhabi. "Eurasian snow cover variability and northern hemisphere climate predictability." Geophysical Research Letters 26, no. 3 (1999): 345–48. http://dx.doi.org/10.1029/1998gl900321.

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Woollings, T., M. Lockwood, G. Masato, C. Bell, and L. Gray. "Enhanced signature of solar variability in Eurasian winter climate." Geophysical Research Letters 37, no. 20 (2010): n/a. http://dx.doi.org/10.1029/2010gl044601.

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Siegert, Martin J., and Isabelle Marsiat. "Numerical reconstructions of LGM climate across the Eurasian Arctic." Quaternary Science Reviews 20, no. 15 (2001): 1595–605. http://dx.doi.org/10.1016/s0277-3791(01)00017-8.

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Hao, Xin, Shengping He, Tingting Han, and Huijun Wang. "Impact of Global Oceanic Warming on Winter Eurasian Climate." Advances in Atmospheric Sciences 35, no. 10 (2018): 1254–64. http://dx.doi.org/10.1007/s00376-018-7216-5.

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