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Journal articles on the topic 'Cold and humid continental climate'

Author: Grafiati

Published: 7 July 2024

Last updated: 31 July 2025

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1

Vivian, Jacopo, Philipp Heer, and Massimo Fiorentini. "Effect of climate on the optimal sizing and operation of seasonal ice storage systems." Journal of Physics: Conference Series 2600, no. 8 (2023): 082021. http://dx.doi.org/10.1088/1742-6596/2600/8/082021.

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Abstract Seasonal thermal storage systems can reduce the temporal mismatch between renewable energy availability and energy demand. Ice storage systems exhibit a non-linear behaviour in the heat exchange and storage processes, complicating the formulation of optimal design and operation problems. In this work, we propose a mixed-integer quadratically-constrained programming formulation, which minimizes the Levelized Cost of Energy for space heating and cooling, including sizing of a supporting PV array. The optimization was repeated for different storage volumes, finding the system optimal ope

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Buric, Dragan, Milan Milenkovic, and Vladan Ducic. "The specificities of the climate of Danilovgrad (Montenegro)." Glasnik Srpskog geografskog drustva 99, no. 1 (2019): 19–28. http://dx.doi.org/10.2298/gsgd1901019b.

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Danilovgrad and the Bjelopavlica Plain belong to the submediterranean zone of the Mediterranean climate region. The aim of this paper was to determine some specific characteristics of the Danilovgrad climate, such as the degree of continentality, aridity and bioclimatic characteristics. Data used in the research cover the period 1955-2011. The results of the study showed the dominance of the continental effect on temperature, while oceanicity was less pronounced. In hygric terms, during most of the year the climate of Danilovgrad is characterized as low humid to perhumid. Moreover, in the peri

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Khan, Saifullah, and Mahmood Ul Hasan. "Climate Classification of Pakistan." International Journal of Economic and Environmental Geology 10, no. 2 (2019): 60–71. http://dx.doi.org/10.46660/ijeeg.vol10.iss2.2019.264.

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The research covenants amid the evaluation and analysis of the weather data in regards to mean monthlytemperature, precipitation, rainy days, relative humidity, wind direction, atmospheric pressure, evaporation, solarradiation and with the literature cited. The components getting fluctuation in the atmospheric condition comprise ofglobal location, vicinity to ocean, geomorphic reliefs and continental extent, maritime affects, forests and landuse.Based on the daily and monthly temperature, the study area has divided into five localities consisting of hot, warm,mild, cool, and cold. Besides, the

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Khan, Saifullah, and Mahmood Ul Hasan. "Climate Classification of Pakistan." International Journal of Economic and Environmental Geology 10, no. 2 (2019): 60–71. http://dx.doi.org/10.46660/ojs.v10i2.264.

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The research covenants amid the evaluation and analysis of the weather data in regards to mean monthlytemperature, precipitation, rainy days, relative humidity, wind direction, atmospheric pressure, evaporation, solarradiation and with the literature cited. The components getting fluctuation in the atmospheric condition comprise ofglobal location, vicinity to ocean, geomorphic reliefs and continental extent, maritime affects, forests and landuse.Based on the daily and monthly temperature, the study area has divided into five localities consisting of hot, warm,mild, cool, and cold. Besides, the

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Ananko, T. V., D. E. Konyushkov, and M. I. Gerasimova. "Palevye soils with a bleached horizon developing from carbonate-free rocks in the classification System of Russian Soils." Dokuchaev Soil Bulletin, no. 87 (March 1, 2017): 22–38. http://dx.doi.org/10.19047/0136-1694-2017-87-22-38.

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The position of palevye soils with differentiated profiles and with podzolized horizons developing from carbonate-free rocks under conditions of the cold extremely continental semihumid climate in the permafrost zone of Central Siberia in the New Russian Classification system is analyzed. The profile of these soils consists of the raw-humus horizon, bleached podzolic or eluvial horizon, and iron-illuvial or clay-illuvial horizon with some features typical of the metamorphic pale soils. According to the character of their middle-profile horizons, they can be attributed to the orders of Al-Fe-hu

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Burjachs, Francesc, and Ramon Julià. "Abrupt Climatic Changes during the Last Glaciation Based on Pollen Analysis of the Abric Romani, Catalonia, Spain." Quaternary Research 42, no. 3 (1994): 308–15. http://dx.doi.org/10.1006/qres.1994.1081.

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AbstractThe Abric Romani continental pollen record provides evidence of abrupt climate variations during the last glaciation. The pollen record reveals a pattern of high-frequency variations similar to that in ice cores as shown by oxygen isotopes or dust content. Analyses of 14 travertine samples yield coherent U-series ages in correct stratigraphic order, ranging from 40,000 to 70,000 yr. According to changes in the composition and structure of the vegetation, five paleoclimatic phases have been differentiated; the oldest, ranging from 70,200 to 65,500 yr ago, records thermophilous taxa whic

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М.В., БОЧАРНИКОВ. "БИОКЛИМАТЫ ВЫСОТНЫХ ПОЯСОВ РАСТИТЕЛЬНОСТИ ГОР РОССИИ". География и природные ресурсы 44, № 2 (2023): 24–36. http://dx.doi.org/10.15372/gipr20230203.

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Проведено биоклиматическое обоснование разнообразия и структуры растительного покрова гор России. На основе выявления климатопов высотно-поясных подразделений, составляющих основу спектров горных систем, и анализа сопряженного развития растительного покрова оробиомов с климатическими условиями определены возможности его формирования в рамках высотных спектров. Для получения опорных биоклиматических показателей использована глобальная модель Chelsa. В число показателей вошли средние многолетние температуры года, июля и января, количество осадков года и июля, значения радиационного баланса; на о

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Lamy, Frank, Dierk Hebbeln, and Gerold Wefer. "High-Resolution Marine Record of Climatic Change in Mid-latitude Chile during the Last 28,000 Years Based on Terrigenous Sediment Parameters." Quaternary Research 51, no. 1 (1999): 83–93. http://dx.doi.org/10.1006/qres.1998.2010.

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AbstractMarine sediment cores from the continental slope off mid-latitude Chile (33°S) were studied with regard to grain-size distributions and clay mineral composition. The data provide a 28,000-yr14C accelerator mass spectrometry-dated record of variations in the terrigenous sediment supply reflecting modifications of weathering conditions and sediment source areas in the continental hinterland. These variations can be interpreted in terms of the paleoclimatic evolution of mid-latitude Chile and are compared to existing terrestrial records. Glacial climates (28,000–18,000 cal yr B.P.) were g

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Zhang, Ningning, Pengyu Cao, Lijing Zhao, Lin Wang, Wangshu Shao, and Rongyu Li. "Effect of temperature fluctuations in cold seasons on acute myocardial infarction hospitalisations in northeast China: a retrospective observational cohort study." BMJ Open 13, no. 11 (2023): e073528. http://dx.doi.org/10.1136/bmjopen-2023-073528.

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ObjectiveThis study aimed to determine the potential influence of ambient temperature on the incidence of acute myocardial infarction (AMI).DesignA retrospective observational cohort study.SettingChangchun, a northeastern city in China, has a temperate continental humid climate.Participants1933 AMI patients admitted to the outpatient department of the First Hospital of Jilin University were included in the study from 1 January 2017 to 31 December 2019.Outcome measureWe explored the effect of daily minimum and maximum temperatures, as well as temperature changes on two adjacent days, on the inc

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Zibzeev, E. G. "High-mountain vegetation of the southern macro-slope of Academician Obruchev Range (East Tuva Plateau)." Vegetation of Russia, no. 12 (2008): 3–20. http://dx.doi.org/10.31111/vegrus/2008.12.3.

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The Academician Obruchev Range is situated between Central Asian and the South Siberian high mountains. Residual influence of western moist air masses, constant influence of southern anticyclone in summer and northern one in winter form the semi-humid climate type of this region. The altitudinal belt vegetation structure of the western and central part of the southern macroslope of the Academician Obruchev Range belong to the East-Tuva semi-humid continental type. The upper limit of forests lies at the altitude about 1800 meters above s. l. The high-mountain belt is subdivided into two flora-c

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Riechelmann, S., D. Buhl, A. Schröder-Ritzrau, et al. "The magnesium isotope record of cave carbonate archives." Climate of the Past 8, no. 6 (2012): 1849–67. http://dx.doi.org/10.5194/cp-8-1849-2012.

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Abstract. Here we explore the potential of magnesium (δ26Mg) isotope time-series data as continental climate proxies in speleothem calcite archives. For this purpose, a total of six Pleistocene and Holocene stalagmites from caves in Germany, Morocco and Peru and two flowstones from a cave in Austria were investigated. These caves represent the semi-arid to arid (Morocco), the warm-temperate (Germany), the equatorial-humid (Peru) and the cold-humid (Austria) climate zones. Changes in the calcite magnesium isotope signature with time are compared against carbon and oxygen isotope records from th

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Riechelmann, S., D. Buhl, A. Schröder-Ritzrau, et al. "The magnesium isotope record of cave carbonate archives." Climate of the Past Discussions 8, no. 3 (2012): 1835–83. http://dx.doi.org/10.5194/cpd-8-1835-2012.

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Abstract. Here we explore the potential of time-series magnesium (δ26Mg) isotope data as continental climate proxies in speleothem calcite archives. For this purpose, a total of six Pleistocene and Holocene stalagmites from caves in Germany, Morocco and Peru and two flowstones from a cave in Austria were investigated. These caves represent the semi-arid to arid (Morocco), the warm-temperate (Germany), the equatorial-humid (Peru) and the cold-humid (Austria) climate zones. Changes in the calcite magnesium isotope signature with time are placed against carbon and oxygen isotope records from thes

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Bassetti, Maria-Angela, Serge Berné, Marie-Alexandrine Sicre, et al. "Holocene hydrological changes in the Rhône River (NW Mediterranean) as recorded in the marine mud belt." Climate of the Past 12, no. 7 (2016): 1539–53. http://dx.doi.org/10.5194/cp-12-1539-2016.

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Abstract. Expanded marine Holocene archives are relatively scarce in the Mediterranean Sea because most of the sediments were trapped in catchment areas during this period. Mud belts are the most suitable targets to access expanded Holocene records. These sedimentary bodies represent excellent archives for the study of sea–land interactions and notably the impact of the hydrological activity on sediment accumulation. We retrieved a 7.2 m long sediment core from the Rhône mud belt in the Gulf of Lions in an area where the average accumulation rate is ca. 0.70 m 1000 yr−1. This core thus provide

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Gagiu, Valeria, Elena Mateescu, Alina Alexandra Dobre, et al. "Deoxynivalenol Occurrence in Triticale Crops in Romania during the 2012–2014 Period with Extreme Weather Events." Toxins 13, no. 7 (2021): 456. http://dx.doi.org/10.3390/toxins13070456.

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This article aims to evaluate deoxynivalenol occurrence in triticale crops in Romania in years with extreme weather events (2012: Siberian anticyclone with cold waves and heavy snowfall; 2013 and 2014: “Vb” cyclones with heavy precipitation and floods in spring). The deoxynivalenol level in triticale samples (N = 236) was quantified by ELISA. In Romania, the extreme weather events favoured deoxynivalenol occurrence in triticale in Transylvania and the southern hilly area (44–47° N, 22–25° E) with a humid/balanced-humid temperate continental climate, luvisols and high/very high risk of floods.

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Finné, Salonen, Frank, et al. "Last Interglacial Climate in Northern Sweden—Insights from a Speleothem Record." Quaternary 2, no. 3 (2019): 29. http://dx.doi.org/10.3390/quat2030029.

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Continental records with absolute dates of the timing and progression of climatic conditions during the Last Interglacial (LIG) from northern Europe are rare. Speleothems from northern Europe have a large potential as archives for LIG environmental conditions since they were formed in sheltered environments and may be preserved beneath ice sheets. Here, we present δ13C and δ18O values from speleothem Kf-21, from Korallgrottan in Jämtland (northwest Sweden). Kf-21 is dated with five MC-ICPMS U-Th dates with errors smaller than ~1 ka. Kf-21 started forming at ~130.2 ka and the main growth phase

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A. Brako, Blestmond, Gordon Foli, Etornam B. Fiadonu, Chiri Amedjoe, Derrick Aikins, and Simon K. Y. Gawu. "PROVENANCE AND TECTONIC SETTING OF SOME PALEOPROTEROZOIC SEDIMENTARY ROCKS IN THE CHAGUPANA AND TARKWA AREAS OF GHANA: PETROGRAPHIC AND STRUCTURAL CONSTRAINTS." Earth Science Malaysia 4, no. 1 (2020): 01–07. http://dx.doi.org/10.26480/esmy.01.2020.01.07.

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Paleoproterozoic sedimentary rocks associated with the Man Shield of West Africa are perceived to be similar, irrespective of their locality. This research seeks to establish the provenance and tectonic setting of these rocks to ascertain any such similarity perception, based on information from two localities. The study uses modal mineral estimations to reconstruct the source, paleocurrent, paleoclimate and relief of some conglomerates and sandstones from Chagupana and Tarkwa areas in Ghana. Chagupana conglomerate has igneous and metamorphic provenances, while Kawere conglomerate has metamorp

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Hou, Haihai, Shujun Liu, Longyi Shao, Yonghong Li, Ming’en Zhao, and Cui Wang. "Elemental geochemistry of the Middle Jurassic shales in the northern Qaidam Basin, northwestern China: Constraints for tectonics and paleoclimate." Open Geosciences 13, no. 1 (2021): 1448–62. http://dx.doi.org/10.1515/geo-2020-0318.

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Abstract The elemental geochemical characteristics of mudstones/shales are good tracers for indicating the evolution of tectonics, paleoenvironment, and paleoclimate. Based on the continuous sampling of drilling cores from the Middle Jurassic Dameigou and Shimengou Formations in the northern Qaidam Basin, the major, trace, and rare earth elements of the 31 mudstones and shales were analyzed. The information on the evolution of tectonics, provenance, and paleoclimate during Middle Jurassic was also recovered. The results show that: (1) A couple of elements consisting of Sc, Y, V, Cr, Co, Ni, Cu

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Maslov, A. V., and V. N. Podkovyrov. "Chemical Weathering Indices and their Use for Paleoclimatic Reconstructions (on the Example of the Vendian‒Lower Cambrian Section of Podolsk Transnistria)." Литология и полезные ископаемые, no. 3 (May 1, 2023): 249–73. http://dx.doi.org/10.31857/s0024497x22700033.

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The article provides an overview of various indices/indicators (Vogt, Parker, CIA, CIW, PIA, MIA, etc.) used in the study of weathering profiles/crusts and reconstruction of paleoclimatic environments of sedimentary sequence accumulation. Their possibilities are demonstrated by the example of Vendian-Lower Cambrian terrigenous deposits of Podolsk Transnistria (southwestern slope of the Ukrainian Shield). The distribution of the ba1 index values in this section indicates the presence of the material most transformed by the processes of chemical weathering in the mudstones of the Nagoryany Forma

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Egorova, Daria A., Olga L. Voronina, Andrey I. Solovyev, et al. "Integrated into Environmental Biofilm Chromobacterium vaccinii Survives Winter with Support of Bacterial Community." Microorganisms 8, no. 11 (2020): 1696. http://dx.doi.org/10.3390/microorganisms8111696.

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Chromobacterium species are common in tropical and subtropical zones in environmental samples according to numerous studies. Here, we describe an environmental case of resident Chromobacterium vaccinii in biofilms associated with Carex spp. roots in Moscow region, Russia (warm-summer humid continental climate zone). We performed broad characterization of individual properties as well as surrounding context for better understanding of the premise of C. vaccinii survival during the winter season. Genome properties of isolated strains propose some insights into adaptation to habit and biofilm mod

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Holcová, Katarína. "Calcareous nannoplankton and foraminiferal response to global Oligocene and Miocene climatic oscillations: a case study from the Western Carpathian segment of the Central Paratethys." Geologica Carpathica 68, no. 3 (2017): 207–28. http://dx.doi.org/10.1515/geoca-2017-0016.

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Abstract The reactions of foraminiferal and calcareous nannoplankton assemblages to global warming and cooling events in the time intervals of ca. 27 to 19 Ma and 13.5 to 15 Ma (Oligocene and Miocene) were studied in subtropical epicontinental seas influenced by local tectonic and palaeogeographic events (the Central Paratethys). Regardless of these local events, global climatic processes significantly influenced the palaeoenvironment within the marine basin. Warm intervals are characterized by a stable, humid climate and a high-nutrient regime, due primarily to increased continental input of

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Jégo, Guillaume, Martin Chantigny, Elizabeth Pattey, et al. "Improved snow-cover model for multi-annual simulations with the STICS crop model under cold, humid continental climates." Agricultural and Forest Meteorology 195-196 (September 2014): 38–51. http://dx.doi.org/10.1016/j.agrformet.2014.05.002.

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Hou, Qinming, and Maohui Luo. "Passive design optimization of shading devices in temperate climate zone method and case studies." Applied and Computational Engineering 136, no. 1 (2025): 19–26. https://doi.org/10.54254/2755-2721/2025.20960.

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This study explores the design thinking behind passive design strategies for building performance optimization, such as shading devices, and demonstrates an integrated workflow. A culinary school in Asheville, North Carolina, is used as a case study. The region has a temperate continental climate with warm, humid summers and cold winters with occasional snowfall. Parametric modeling was performed using the Pollination plug-in in Rhino, and energy simulation was performed using DesignBuilder, while daylight analysis was performed using Ladybug. In order to verify the performance of shading devi

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Lin, Donglin, Shuheng Tang, Zhaodong Xi, Bing Zhang, and Yapei Ye. "Geochemical Characteristics of Late Ordovician Shales in the Upper Yangtze Platform, South China: Implications for Redox Environmental Evolution." Minerals 11, no. 7 (2021): 710. http://dx.doi.org/10.3390/min11070710.

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Changes to the redox environment of seawater in the Late Ordovician affect the process of organic matter enrichment and biological evolution. However, the evolution of redox and its underlying causes remain unclear. This paper analyzed the vertical variability of main, trace elements and δ34Spy from a drill core section (well ZY5) in the Upper Yangtze Platform, and described the redox conditions, paleoproductivity and paleoclimate variability recorded in shale deposits of the P. pacificus zone and M. extraordinarius zone that accumulated during Wufeng Formation. The results showed that shale f

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Hadiwijaya, Bram, Steeve Pepin, Pierre-Erik Isabelle, and Daniel F. Nadeau. "The Dynamics of Transpiration to Evapotranspiration Ratio under Wet and Dry Canopy Conditions in a Humid Boreal Forest." Forests 11, no. 2 (2020): 237. http://dx.doi.org/10.3390/f11020237.

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Humid boreal forests are unique environments characterized by a cold climate, abundant precipitation, and high evapotranspiration. Transpiration ( E T ), as a component of evapotranspiration (E), behaves differently under wet and dry canopy conditions, yet very few studies have focused on the dynamics of transpiration to evapotranspiration ratio ( E T / E ) under transient canopy wetness states. This study presents field measurements of E T / E at the Montmorency Forest, Québec, Canada: a balsam fir boreal forest that receives ∼ 1600 mm of precipitation annually (continental subarctic climate;

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Biste, Michael, and Andrés Burgoa. "NUEVOS ASPECTOS GEOLÓGICO-MINEROS SOBRE EL YACIMIENTO DE BOLIVIANITA ANAHÍ, UBICADO EN EL ORIENTE BOLIVIANO." Boletim do Museu de Geociências da Amazônia 10, no. 2 (2023): 1–4. http://dx.doi.org/10.31419/issn.2594-942x.v102023i2boliviaa11mb.

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A recent investigation of the bolivianita Anahi mine reveals that the mineralization is the product of intracratonic thermal fluids which migrated along a deep lineament and through a basin with an Upper Proterozoic sediment filling. The mineralization is hosted by Cambrian limestone and related to a collapse structure. It occurs within caverns of dissolution, fractures and open spaces which were formed by karstic processes and circulation of thermal fluids. The different types of quartz precipitated by mixing of ascendant thermal fluids enriched in silica with descendent cold meteoric water c

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Berardi, Umberto. "The BeTOP facility for performance testing of building systems." E3S Web of Conferences 396 (2023): 03030. http://dx.doi.org/10.1051/e3sconf/202339603030.

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Proposing new materials and systems to improve buildings' performance and energy efficiency often requires testing their performance in the field. Experimental performance characterization of new and existing building systems is crucial to understanding their behaviour. Full-scale experimental test cell facilities have been at the forefront of experimental performance evaluation in building-related research, as they provide a realistic representation of buildings, including environmental conditions, assembling challenges, and operational characteristics. In this paper, trends in the design and

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Ravelojaona, Nomena, Guillaume Jégo, Noura Ziadi, et al. "STICS Soil–Crop Model Performance for Predicting Biomass and Nitrogen Status of Spring Barley Cropped for 31 Years in a Gleysolic Soil from Northeastern Quebec (Canada)." Agronomy 13, no. 10 (2023): 2540. http://dx.doi.org/10.3390/agronomy13102540.

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Spring barley (Hordeum vulgare L.) is an increasingly important cash crop in the province of Quebec (Canada). Soil–crop models are powerful tools for analyzing and supporting sustainable crop production. STICS model has not yet been tested for spring barley grown over several decades. This study was conducted to calibrate and evaluate the STICS model, without annual reinitialization, for predicting aboveground biomass and N nutrition attributes at harvest during 31 years of successive cropping of spring barley grown in soil (silty clay, Humic Gleysol) from the Saguenay–Lac-Saint-Jean region (n

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Laita, Elisa, Blanca Bauluz, Marcos Aurell, Beatriz Bádenas, José Ignacio Canudo, and Alfonso Yuste. "A change from warm/humid to cold/dry climate conditions recorded in lower Barremian clay-dominated continental successions from the SE Iberian Chain (NE Spain)." Sedimentary Geology 403 (June 2020): 105673. http://dx.doi.org/10.1016/j.sedgeo.2020.105673.

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Satosina, Elizaveta, Nurdin Mamadiev, Lyubov Makhmudova, and Julia Kurbatova. "Carbon Dioxide and Heat Fluxes during Reforestation in the North Caucasus." Forests 14, no. 12 (2023): 2368. http://dx.doi.org/10.3390/f14122368.

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Human impact on natural ecosystems has significantly increased in recent decades. As a result, the structure and functioning of ecosystems are seriously altered. This in turn affects regional weather and climate conditions through changes in the radiation, water, and carbon balance of ecosystems. Investigating the process of natural ecosystem restoration after disturbances is an important issue in the context of climate change. During monitoring observations of greenhouse gas (GHG) fluxes in a reforestation area in the Chechen Republic, new experimental data on their seasonal variability were

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Gastaldo, Robert A., Kaci Kus, Neil Tabor, and Johann Neveling. "Calcic Vertisols in the upper Daptocephalus Assemblage Zone, Balfour Formation, Karoo Basin, South Africa: Implications for Late Permian Climate." Journal of Sedimentary Research 90, no. 6 (2020): 609–28. http://dx.doi.org/10.2110/jsr.2020.32.

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ABSTRACT The fully continental succession of the Beaufort Group, Karoo Basin, South Africa, has been used in the development of environmental models proposed for the interval that spans the contact between the Daptocephalus to Lystrosaurus Assemblage Zones, associated by some workers with the end-Permian extinction event. An aridification trend is widely accepted, yet geochemical data indicate that the majority of in situ paleosols encountered in this interval developed in waterlogged environments. To date, the presence of calcic paleosols in the latest Permian can be inferred only from the pr

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Anonymous. "Peer review report 1 On “Improved snow-cover model for multi-annual simulations with the STICS crop model under cold, humid continental climates”." Agricultural and Forest Meteorology 201 (January 2015): 349. http://dx.doi.org/10.1016/j.agrformet.2015.08.236.

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Mary, Bruno. "Peer review report 2 On “Improved snow-cover model for multi-annual simulations with the STICS crop model under cold, humid continental climates”." Agricultural and Forest Meteorology 201 (January 2015): 365–66. http://dx.doi.org/10.1016/j.agrformet.2015.08.237.

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Naz, Bibi S., Wendy Sharples, Yueling Ma, Klaus Goergen, and Stefan Kollet. "Continental-scale evaluation of a fully distributed coupled land surface and groundwater model, ParFlow-CLM (v3.6.0), over Europe." Geoscientific Model Development 16, no. 6 (2023): 1617–39. http://dx.doi.org/10.5194/gmd-16-1617-2023.

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Abstract. High-resolution large-scale predictions of hydrologic states and fluxes are important for many multi-scale applications, including water resource management. However, many of the existing global- to continental-scale hydrological models are applied at coarse resolution and neglect more complex processes such as lateral surface and groundwater flow, thereby not capturing smaller-scale hydrologic processes. Applications of high-resolution and physically based integrated hydrological models are often limited to watershed scales, neglecting the mesoscale climate effects on the water cycl

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Yartsev, G. F., R. K. Baikasenov, A. A. Kolesnikov, A. T. Akhmetgaliev, and Yu Yu Episheva. "Improvement of elements of cultivation technology for winter crops and chickpea on chernozems of southern and dark chestnut soils of the Orenburg region." IOP Conference Series: Earth and Environmental Science 1206, no. 1 (2023): 012034. http://dx.doi.org/10.1088/1755-1315/1206/1/012034.

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Abstract The Orenburg region is characterized by a sharp continental climate. It is characterized by cold winters, and frequent droughts in summer. That is why, the most frost-resistant winter wheat and rye of winter crops are cultivated in the region, and the chickpea is the most drought-resistant one of grain legumes. The changing climate requires constant clarification of sowing dates, methods, seeding rates, and emerging new liquid fertilizers require clarification, if possible, of their joint application in certain phases of plant development. In our winter wheat studies, various combinat

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Rozhanskaya, O. A., and E. M. Gorshkova. "In vitro culture as a source of biodiversity for soybean breeding." Siberian Herald of Agricultural Science 49, no. 4 (2019): 24–31. http://dx.doi.org/10.26898/0370-8799-2019-4-3.

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The paper shows the effectiveness of methods of somaclonal variability in combination with multiple individual selection for creating new soybean varieties characterized by early ripeness and increased seed productivity for sub-arid regions of Russia and Kazakhstan with cold continental climate. Soybean breeding material was created using biotechnology methods combined with multiple individual selection. Higher regeneration potential of soybean tissues of SibNIIK 315 variety compared to Omskaya-4 variety was revealed. The ability to regenerate is associated with the adaptability of SibNIIK 315

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Varela, Luciano, and Richard A. Fariña. "Co-occurrence of mylodontid sloths and insights on their potential distributions during the late Pleistocene." Quaternary Research 85, no. 1 (2016): 66–74. http://dx.doi.org/10.1016/j.yqres.2015.11.009.

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Species distribution models (SDMs) for the last interglacial (LIG), the global last glacial maximum (LGM) and the Holocene climatic optimum (HCO) were generated for three extinct South American Pleistocene mylodontid giant sloths,Glossotherium robustum,Lestodon armatusandMylodon darwinii. They are recorded co-occurring in some localities including Arroyo del Vizcaíno site (AdV) in Uruguay. Co-occurrence records were studied based on the overlap of their generated areas of potential distributions, and compared with the available biome reconstructions of South America during the LGM to analyze t

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SR, Bhadra Kumary, Gopakumar B, Manjunatha BR, Anil Kumar A, Shaniba V та Subhradeep Das. "Glacial-Interglacial Cycles over the Past 150,000 years of South-Eastern Arabian Sea from δ18O Record". Journal of Research in Environmental and Earth Sciences 10, № 11 (2024): 09–21. http://dx.doi.org/10.35629/2532-10110921.

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This study aims to reconstruct the surface water productivity and related monsoonal intensity along the southwestern continental margin of India, over the last 150,000 years by utilizing the temporal variations of δ18O and δ13C isotopes in the planktic foraminifers (Globigerinoides ruber) from a sediment core obtained from the continental slope off Kochi, south-eastern India. The chronostratigraphy of the core is established on the basis of high resolution stable isotope record of planktic foraminifera (Globigerinoides ruber) and a few AMS radiocarbon ages. Down-core records of δ18O and δ13C s

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SR, Bhadra Kumary, Gopakumar B, Manjunatha BR, Anil Kumar A, Shaniba V та Subhradeep Das. "Glacial-Interglacial Cycles over the Past 150,000 years of South-Eastern Arabian Sea from δ18O Record". Journal of Research in Environmental and Earth Sciences 10, № 11 (2024): 22–34. http://dx.doi.org/10.35629/2532-10112234.

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This study aims to reconstruct the surface water productivity and related monsoonal intensity along the southwestern continental margin of India, over the last 150,000 years by utilizing the temporal variations of δ18O and δ13C isotopes in the planktic foraminifers (Globigerinoides ruber) from a sediment core obtained from the continental slope off Kochi, south-eastern India. The chronostratigraphy of the core is established on the basis of high resolution stable isotope record of planktic foraminifera (Globigerinoides ruber) and a few AMS radiocarbon ages. Down-core records of δ18O and δ13C s

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Ye, S., M. A. Yaeger, E. Coopersmith, L. Cheng, and M. Sivapalan. "Exploring the physical controls of regional patterns of flow duration curves – Part 2: Role of seasonality and associated process controls." Hydrology and Earth System Sciences Discussions 9, no. 6 (2012): 7035–84. http://dx.doi.org/10.5194/hessd-9-7035-2012.

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Abstract. The goal of this paper is to explore the process controls underpinning regional patterns of variations of runoff regime behavior, i.e., the mean seasonal variation of runoff within the year, across the continental United States. The ultimate motivation is to use the resulting process understanding to generate insights into the physical controls of Flow Duration Curves, in view of the close connection between these two alternative signatures of runoff variability. To achieve these aims a top-down modeling approach is adopted; we start with a simple two-stage bucket model, which is sys

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Musil, Rudolf. "Phenological Analysis of the Last Glacial Vertebrates from the Territory of Moravia (the Czech Republic) – Continuity and Change in Faunistic Communities." Fossil Imprint 74, no. 3-4 (2018): 199–236. http://dx.doi.org/10.2478/if-2018-0015.

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Due to the vertical zonality of the studied area, its environment varied greatly over a relatively short distance within the same time span. It is possible to distinguish the following different types of environment: (1) Alluvial floodplains around larger water flows. I assume in the Last Glacial there was continuous coniferous forest, with occasional sporadic occurrences of thermophilous deciduous trees in favourable locations mainly in south Moravia. (2) Lower foothills up to about 300 m a.s.l. along the floodplains, probably the most widespread type of environment in the studied area. Open

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Belonovskaya, E. A., V. V. Vinogradova, M. A. Ponomaryov, A. A. Tishkov, and N. G. Tsarevskaya. "Evaluating the recreation potential of the national park “Valdayskiy” (Novgorodskaya Oblast, Russia)." Izvestiya Rossiiskoi akademii nauk. Seriya geograficheskaya, no. 4 (August 28, 2019): 97–111. http://dx.doi.org/10.31857/s2587-55662019497-111.

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The National Park “Valdayskiy” (the Park) was established to preserve the unique lake-forest complex of the Valday upland and to create conditions for the development of organized recreation on this territory. Incomparable beautiful views of different landscapes attracthere thousands of tourists from various Russian regions.The greater number of them prefers lakeshores for camping,so special attention in the research was paid tothe studyofriparian and shallow water vegetation of lakesin zones with different recreation pressureto establish the patterns of vegetation digression.The materials of

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Ye, S., M. Yaeger, E. Coopersmith, L. Cheng, and M. Sivapalan. "Exploring the physical controls of regional patterns of flow duration curves – Part 2: Role of seasonality, the regime curve, and associated process controls." Hydrology and Earth System Sciences 16, no. 11 (2012): 4447–65. http://dx.doi.org/10.5194/hess-16-4447-2012.

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Abstract. The goal of this paper is to explore the process controls underpinning regional patterns of variations of streamflow regime behavior, i.e., the mean seasonal variation of streamflow within the year, across the continental United States. The ultimate motivation is to use the resulting process understanding to generate insights into the physical controls of another signature of streamflow variability, namely the flow duration curve (FDC). The construction of the FDC removes the time dependence of flows. Thus in order to better understand the physical controls in regions that exhibit st

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Bos, Johanna A. A., and Bas van Geel. "Palaeoenvironmental reconstruction based on the Early Holocene Haelen sequence, near Roermond (southeastern Netherlands)." Netherlands Journal of Geosciences 96, no. 2 (2016): 115–30. http://dx.doi.org/10.1017/njg.2016.35.

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AbstractHigh-resolution Early Holocene palynological records from the middle Meuse River valley were missing until recently. In order to investigate environmental and inferred climate changes during the Preboreal, sediments from a former residual channel of the Meuse River near Haelen were studied. Detailed multi-proxy analyses, including microfossils, macroremains and loss-on-ignition measurements, were carried out at a high temporal resolution. An accurate chronology of the >1000-year-long record was provided by accelerator mass spectrometry (AMS)14C wiggle-match dating.The channel was ab

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Narloch, Piotr, and Piotr Woyciechowski. "Assessing Cement Stabilized Rammed Earth Durability in A Humid Continental Climate." Buildings 10, no. 2 (2020): 26. http://dx.doi.org/10.3390/buildings10020026.

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The article compared the test results of a number of features determining the durability of rammed earth durability in a humid continental climate. The results of wet to dry compressive strength ratio, frost resistance, linear shrinkage, resistance to erosion under the influence of a stream of pressurized water, and resistance to erosion under the influence of cyclic wetting and drying were presented. All of the tests were done on the same soil-cement mixture. On this basis, it was determined which of the methods of durability assessment is more and which is less restrictive. A new method for

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MOBASSHER, A., and AHMAD HOSSAIN. "Climatic classification of Bangladesh." MAUSAM 46, no. 1 (2022): 25–30. http://dx.doi.org/10.54302/mausam.v46i1.3153.

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Using climatological data for 27 years of 16 stations an attempt has been made to classify the climate of Bangladesh by the method of Ivanov (1941. 1956 & 1958). Selianinov (1966). Gorsinkii and Shever (1976). By Ivanov's method it has been established that there are three climatic zones in Bangladesh (i) zone with simple humid climate- western bordering districts of Bangladesh; (ii) zone with sufficient humid climate -areas of Bangladesh mainly to the west of 90. E and (iii) zone with super humid climate areas or Bangladesh mainly to the east of 90"E. Almost analogous climatic zones have

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Liu, Da Long, Jia Ping Liu, and Liu Yang. "Building Climatic Classification in China." Advanced Materials Research 374-377 (October 2011): 365–68. http://dx.doi.org/10.4028/www.scientific.net/amr.374-377.365.

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Different climate bring about different buildings, Climate has very close relation with architecture. Building climatic classification has important direction mean for architecture design, building energy efficiency and building energy simulation. Ago, China classified building climate using temperature, relative humidity, etc.. Degree, relative humidity and clearness index were regarded as classification factors. Meteorological data of 165 stations from 1970 to 2000 is used to reclassify building climate in China. Six types of building climates which respectively is Warm, Warm & humid, We

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Blyakharchuk, T. A., N. V. Shefer, E. A. Lukanina, M. Van Hardenbroek, S. Juggins, and D. Zhang. "Modern spore-pollen spectra of the Altai-Sayan region, their relationship with climate and transfer functions for palaeoclimate reconstructions." Environmental Dynamics and Global Climate Change 15, no. 2 (2024): 82–97. http://dx.doi.org/10.18822/edgcc635871.

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Quantitative reconstruction of paleoclimate based on spore-pollen data remains an important task in the study of long-term climate dynamics. The construction of transfer pollen-climate functions on a training set of modern spore-pollen spectra is an effective method for such studies, especially necessary in areas that are poorly supported by numerical reconstructions of paleoclimate, which includes Siberia. To solve this problem, a series of 145 modern spore-pollen spectra were collected during summer expedition at different years from various phytocenoses (plant functional types) representing

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Baghaiepoor, Mahtab, Goran Jovanovic, and Mirko Stanimirovic. "Climate adapted houses in Iran: Hot, cold and humid climate." Facta universitatis - series: Architecture and Civil Engineering 17, no. 4 (2019): 429–43. http://dx.doi.org/10.2298/fuace180721025b.

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The issue of Climate Change has raised so much attention for decades, specifically in recent years. Modern trends in urban architecture which tried to create living machines similar to each other in any context, have now been proven to be insufficient and unless we decide to respect nature and make our buildings cooperate with their contexts as soon as possible we cannot address further threads regarding our future life. If we take a look at traditional architecture existing in old towns and rural area, we can see how people managed to bond a new construction with its surroundings. In this art

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Park, Chang-Eui, Su-Jong Jeong, Chang-Hoi Ho, et al. "Dominance of climate warming effects on recent drying trends over wet monsoon regions." Atmospheric Chemistry and Physics 17, no. 17 (2017): 10467–76. http://dx.doi.org/10.5194/acp-17-10467-2017.

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Abstract. Understanding changes in background dryness over land is key information for adapting to climate change because of its critical socioeconomic consequences. However, causes of continental dryness changes remain uncertain because various climate parameters control dryness. Here, we verify dominant climate variables determining dryness trends over continental eastern Asia, which is characterized by diverse hydroclimate regimes ranging from arid to humid, by quantifying the relative effects of changes in precipitation, solar radiation, wind speed, surface air temperature, and relative hu

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Dong, Meiqi, Jin Zhao, E. Li, et al. "Effects of Changing Climate Extremes on Maize Grain Yield in Northeast China." Agronomy 13, no. 4 (2023): 1050. http://dx.doi.org/10.3390/agronomy13041050.

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The increased frequency of climate extremes associated with ongoing climate change has the potential for significant impacts on maize grain yield in maize-producing regions worldwide. In this study, we used a modeling approach to investigate the effects of different types of climatic extremes on maize grain yield in Northeast China. We combined annual mean air temperature and accumulated precipitation data and divided the climate years into 9 categories, using the 10th and 90th percentiles as extreme thresholds. The climate data were represented by 1 normal climate type, 4 individual climate e

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