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Journal articles on the topic 'Atmosphere-lake interaction'

Author: Grafiati

Published: 11 March 2023

Last updated: 31 July 2025

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1

Djolov, G. "Hydrothermodynamic interaction between lake and atmosphere." Boundary-Layer Meteorology 61, no. 1-2 (1992): 205. http://dx.doi.org/10.1007/bf02034003.

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Wang, Mengxiao, Lijuan Wen, Zhaoguo Li, et al. "Mechanisms and effects of under-ice warming water in Ngoring Lake of Qinghai–Tibet Plateau." Cryosphere 16, no. 9 (2022): 3635–48. http://dx.doi.org/10.5194/tc-16-3635-2022.

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Abstract. The seasonal ice cover in lakes of the Qinghai–Tibet Plateau is a transient and vulnerable part of the cryosphere, whose characteristics depend on the regional climate: strong solar radiation in the context of the dry and cold environment because of the high altitude and relatively low latitude. We use the first under-ice temperature observations from the largest Tibetan freshwater lake, Ngoring Lake, and a one-dimensional lake model to quantify the mechanism of solar thermal accumulation under ice, which relies on the ice optical properties and weather conditions, as well as the eff

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Turchak, Leonid I., and Maria I. Gritsevich. "Meteoroids Interaction With The Earth Atmosphere." Journal of Theoretical and Applied Mechanics 44, no. 4 (2014): 15–28. http://dx.doi.org/10.2478/jtam-2014-0020.

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Abstract In this study we evaluate meteoroid mass and its other properties based on the observed atmospheric trajectory. With account for aerodynamics, we formulate a problem by introducing key dimensionless parameters in the model, responsible for the drag, mass loss and rotation of meteoroid. The proposed model is suitable to categorize various impact events in terms of meteor survivability and impact damage and thus, to analyze consequences that accompany collisions of cosmic bodies with planetary atmosphere and surface. The different types of events, namely, formation of a massive single c

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Gao, Yanhong, Fei Chen, Gonzalo Miguez-Macho, and Xia Li. "Understanding precipitation recycling over the Tibetan Plateau using tracer analysis with WRF." Climate Dynamics 55, no. 9-10 (2020): 2921–37. http://dx.doi.org/10.1007/s00382-020-05426-9.

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Abstract The precipitation recycling (PR) ratio is an important indicator that quantifies the land-atmosphere interaction strength in the Earth system’s water cycle. To better understand how the heterogeneous land surface in the Tibetan Plateau (TP) contributes to precipitation, we used the water-vapor tracer (WVT) method coupled with the Weather Research and Forecasting (WRF) regional climate model. The goals were to quantify the PR ratio, in terms of annual mean, seasonal variability and diurnal cycle, and to address the relationships of the PR ratio with lake treatments and precipitation am

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Specht, Nora Farina, Martin Claussen, and Thomas Kleinen. "Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene." Climate of the Past 20, no. 7 (2024): 1595–613. http://dx.doi.org/10.5194/cp-20-1595-2024.

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Abstract. During the early Holocene to mid-Holocene, about 11 500 to 5500 years ago, lakes expanded across the Sahel and Sahara in response to enhanced summer monsoon precipitation. To investigate the effect of these lakes on the West African summer monsoon, previous simulation studies prescribed mid-Holocene lakes from reconstructions. By prescribing mid-Holocene lakes, however, the terrestrial water balance is inconsistent with the size of the lakes. In order to close the terrestrial water cycle, we construct a dynamic endorheic lake (DEL) model and implement it into the atmosphere–land mode

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Хайретдинов, М. С., В. В. Ковалевский та Г. М. Шиманская. "Вибрационные волны в системе литосфера - атмосфера - гидросфера". Вычислительные технологии 30, № 3 (2025): 37–46. https://doi.org/10.25743/ict.2025.30.3.004.

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Предложен интегрированный подход к решению проблемы изучения взаимодействия инфранизкочастотных геофизических волновых полей разной природы (сейсмических, акустических и гидроакустических) от природных и техногенных источников с учетом метеофакторов. В качестве источников волновых полей в экспериментах рассматриваются сейсмические вибраторы, обладающие свойством порождать одновременно сейсмические волны в земле и акустические в атмосфере. Высокая повторяемость волновых форм в экспериментах с применением таких источников обеспечивает высокие метрологическую точность и разрешающую способность в

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Wardani, Alvia Rahma, Aulia Benazira, and Nella Anggreini. "Pengaruh Karakteristik Event terhadap Keputusan Berkunjung di The Kaldera Nomadic Escape Studi Kasus : Event Marende Fest 2024." Abdimas Indonesian Journal 4, no. 2 (2024): 343–50. https://doi.org/10.59525/aij.v4i2.461.

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The Caldera Nomadic Escape is a tourist destination developed by the Ministry of Tourism through the Lake Toba Authority Implementing Agency (BPODT). This research aims to determine the influence of event characteristics on the decision to visit domestic tourists at The Kaldera Nomadic Escape case study: Marende Fest 2024 event. The population of this study was 2,463 and the sample used was 100 respondents. The sampling technique used was nonprobability sampling with purposive sampling technique. This research uses quantitative research methods with a descriptive research type which includes v

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Chen, Haishan, Bo Yu, Botao Zhou, Wanxin Zhang, and Jie Zhang. "Role of Local Atmospheric Forcing and Land–Atmosphere Interaction in Recent Land Surface Warming in the Midlatitudes over East Asia." Journal of Climate 33, no. 6 (2020): 2295–309. http://dx.doi.org/10.1175/jcli-d-18-0856.1.

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AbstractSignificant summer land surface warming has been observed in the middle latitudes over East Asia, especially after the mid-1990s, which has evidently affected the East Asian weather and climate. Using multisource observations and reanalysis data during 1979–2013, this study explores the possible reasons for recent land surface warming over this region by considering atmospheric forcing and regional land–atmosphere interaction related to extratropical cyclones (ECs). Results show that there is a close relationship between land surface warming and weakened ECs over East Asia. Recent land

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Gemilang, Annisa, Huda Nurjanti, and Firmansam Bastaman. "Lanskap Agrowisata Kopi Sumedang Sebagai Kolaborasi Peningkatan Perkebunan Rakyat Dan Perlindungan Lahan Danau Sunyayuri." Composite: Jurnal Ilmu Pertanian 3, no. 02 (2021): 68–77. http://dx.doi.org/10.37577/composite.v3i02.361.

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called Kopi Buhun. Buhun Coffee is a type of Arabica coffee which is a single origin "special tea coffee". In developing Buhun coffee, land is needed that can be planted with coffee. This land is not only a coffee plantation but can become a tourist attraction that can educate, increase recreation and protect the environment besides that it can economically increase the income of residents around agrotourism. In general, the land of Lake Sunyayuri, Cimarias Village, Pamulihan District, Sumedang Regency is an area that has the potential to become a tourist spot with an artificial lake, and a pa

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Benelli, Sara, Bianca Maria Lecchini, Chiara Montecorboli, Clara Spicer, and Marco Bartoli. "Greenhouse gas fluxes in an oxbow lake and its exposed sediments during periods of hydraulic connection and disconnection." ARPHA Conference Abstracts 8 (May 28, 2025): e149540. https://doi.org/10.3897/aca.8.e149540.

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After decades of systematic simplification of river ecosystems through hydraulic interventions that have reduced the interactions between the river and its floodplain, projects are now underway to reconnect rivers with riparian areas and lateral canals. The navigation groynes separating the Po River from the Gussola oxbow lake (Cremona, northern Italy) underwent a requalification intervention in March 2023, which consisted of lowering them in order to increase the frequency of flooding and, consequently, the interaction between the river and the oxbow lake. Before and after the requalification

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Jiang, Haoyu, Yingyao He, Yiqun Wang, et al. "Formation of organic sulfur compounds through SO<sub>2</sub>-initiated photochemistry of PAHs and dimethylsulfoxide at the air-water interface." Atmospheric Chemistry and Physics 22, no. 6 (2022): 4237–52. http://dx.doi.org/10.5194/acp-22-4237-2022.

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Abstract. The presence of organic sulfur compounds (OS) at the water surface acting as organic surfactants, may influence the air-water interaction and contribute to new particle formation in the atmosphere. However, the impact of ubiquitous anthropogenic pollutant emissions, such as SO2 and polycyclic aromatic hydrocarbons (PAHs) on the formation of OS at the air-water interface still remains unknown. Here, we observe large amounts of OS formation in the presence of SO2, upon irradiation of aqueous solutions containing typical PAHs, such as pyrene (PYR), fluoranthene (FLA), and phenanthrene (

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Pickarski, N., O. Kwiecien, D. Langgut, and T. Litt. "Abrupt climate and vegetation variability of eastern Anatolia during the last glacial." Climate of the Past 11, no. 11 (2015): 1491–505. http://dx.doi.org/10.5194/cp-11-1491-2015.

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Abstract. Detailed analyses of the Lake Van pollen, Ca / K ratio, and stable oxygen isotope record allow the identification of millennial-scale vegetation and environmental changes in eastern Anatolia throughout the last glacial (~ 111.5–11.7 ka BP). The climate of the last glacial was cold and dry, indicated by low arboreal pollen (AP) levels. The driest and coldest period corresponds to Marine Isotope Stage (MIS) 2 (~ 28–14.5 ka BP), which was dominated by highest values of xerophytic steppe vegetation. Our high-resolution multi-proxy record shows rapid expansions and contractions of tree po

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Pickarski, N., O. Kwiecien, D. Langgut, and T. Litt. "Abrupt climate variability of eastern Anatolia vegetation during the last glacial." Climate of the Past Discussions 11, no. 4 (2015): 3341–73. http://dx.doi.org/10.5194/cpd-11-3341-2015.

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Abstract. Detailed analyses of the Lake Van pollen and stable oxygen isotope record allow the identification of millennial-scale vegetation and environmental changes in eastern Anatolia throughout the last glacial. The climate within the last glacial period (∼75–15 ka BP) was cold and dry, with low arboreal pollen (AP) levels. The driest and coldest period corresponds to Marine Isotope Stage (MIS) 2 (∼28–14.5 ka BP) dominated by the highest values of xerophytic steppe vegetation. Our high-resolution multi proxy record shows rapid expansions and contractions that mimic the stadial-interstadial

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Rúa, Alex, Jaime Palacio Baena, and María Teresa Flórez Molina. "Relation of hydrological pulse to sediment stratigraphy in the Ayapel Flood Plain Lake, Colombia." Revista Facultad de Ingeniería Universidad de Antioquia, no. 70 (February 27, 2014): 197–206. http://dx.doi.org/10.17533/udea.redin.18663.

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The hydrological pulse and matter transfer between tributaries and wetlands link terrestrial and rheotrophic environments. The water-sediment interaction on multidecadal scale within wetlands of Colombian Atlantic savannahs remains greatly unknown. This study stratigraphically correlated nine sediment cores (13-30 cm) spanning ca. 110-600 years BP from the Ayapel Flood Plain Lake (AFPL). These correlations framed (i) zones of high anthropogenic pressure, (ii) main hydrodynamics, and (iii) organic matter (OM) contributions. More than 84% out of the 150 km2-extension of the AFPL was comprised of

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Pandey, Siddharth, Jonathan Clarke, Preeti Nema, et al. "Ladakh: diverse, high-altitude extreme environments for off-earth analogue and astrobiology research." International Journal of Astrobiology 19, no. 1 (2019): 78–98. http://dx.doi.org/10.1017/s1473550419000119.

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AbstractThis paper highlights unique sites in Ladakh, India, investigated during our 2016 multidisciplinary pathfinding expedition to the region. We summarize our scientific findings and the site's potential to support science exploration, testing of new technologies and science protocols within the framework of astrobiology research. Ladakh has several accessible, diverse, pristine and extreme environments at very high altitudes (3000–5700 m above sea level). These sites include glacial passes, sand dunes, hot springs and saline lake shorelines with periglacial features. We report geological

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Sari, Siti Khairani P., Muhammad Rais Abdillah, Ivonne M. Radjawane, Dwina Nugraha, and Syahandra Ramadhan. "Impact of ENSO on the Variability of Electricity Production at a Hydropower Plant in Bakaru Sulawesi, Indonesia." IOP Conference Series: Earth and Environmental Science 1472, no. 1 (2025): 012026. https://doi.org/10.1088/1755-1315/1472/1/012026.

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Abstract El Niño-Southern Oscillation (ENSO) is a large-scale interaction of ocean and atmosphere that manifests itself as fluctuations in ocean surface temperature and air pressure in the tropical Pacific Ocean. The impact of ENSO has been felt worldwide, including in the energy sector. Changes in sea surface temperature and rainfall patterns can affect the drainage of river and lake water used for hydroelectric power generation. Hydropower Plant is one type of power plant that uses potential energy of water into kinetic energy which is then used to move turbines and generate electricity. Her

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17

Conry, Patrick, Ashish Sharma, Mark J. Potosnak, et al. "Chicago’s Heat Island and Climate Change: Bridging the Scales via Dynamical Downscaling." Journal of Applied Meteorology and Climatology 54, no. 7 (2015): 1430–48. http://dx.doi.org/10.1175/jamc-d-14-0241.1.

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AbstractThe interaction of global climate change and urban heat islands (UHI) is expected to have far-reaching impacts on the sustainability of the world’s rapidly growing urban population centers. Given that a wide range of spatiotemporal scales contributed by meteorological forcing and complex surface heterogeneity complicates UHI, a multimodel nested approach is used in this paper to study climate-change impacts on the Chicago, Illinois, UHI, covering a range of relevant scales. One-way dynamical downscaling is used with a model chain consisting of global climate (Community Atmosphere Model

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18

Ganbat, Danaa, and Gantuya Ganbat. "Results of simulations of atmosphere-lake interactions using numerical model." Embedded Selforganising Systems 9, no. 3 (2022): 37–38. http://dx.doi.org/10.14464/ess.v9i3.535.

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Lakes influence the regional atmosphere through modifying thermodynamic characteristics. This study examines the effects of the Baikal lake on meteorological parameters in summertime using the numerical model. Diurnal variations in the lakes’ impact on the atmosphere are found through changing the surface energy budget, which includes changes in sensible and latent heat fluxes. The changes in heat fluxes cause relatively lower surface temperature which leads to a shallow boundary layer over the lake surfaces. Greater heat capacity in water bodies compared to grasslands causes slower heating an

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Santisteban, María, Ana Teresa Luís, José Antonio Grande, et al. "Hydrochemical Characterization of an Acid Mine Effluent from Concepcion Mine Using Classical Statistic and Fuzzy Logic Techniques." Minerals 12, no. 4 (2022): 464. http://dx.doi.org/10.3390/min12040464.

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This work focuses on the physical-chemical characterization of a mining effluent affected by acid mine drainage (AMD) from its source to the confluence in the Odiel river, one of the most polluted rivers by AMD worldwide, in order to understand the reactions involved in the modifications in the chemical characteristics of water and precipitates resulting from water–rock–atmosphere interaction in an environment highly affected by mining activity without corrective measures. The channel starts in an open pit lake through one of the Concepción Mine main galleries, located in the Iberian Pyrite Be

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Laiti, L., D. Zardi, M. de Franceschi, and G. Rampanelli. "Analysis of the diurnal development of the <i>Ora del Garda</i> wind in the Alps from airborne and surface measurements." Atmospheric Chemistry and Physics Discussions 13, no. 7 (2013): 19121–71. http://dx.doi.org/10.5194/acpd-13-19121-2013.

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Abstract. A lake-breeze and valley-wind coupled circulation system, known as Ora del Garda, typically arises in the late morning from the northern shorelines of Lake Garda (southeastern Italian Alps), and then channels into the Sarca and Lakes valleys to the north. After flowing over an elevated saddle, in the early afternoon this wind breaks out from the west into the nearby Adige Valley, hindering the regular development of the local up-valley wind by producing a strong and gusty anomalous flow in the area. Two targeted flights of an equipped motorglider were performed in the morning and aft

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Huziy, O., and L. Sushama. "Lake–river and lake–atmosphere interactions in a changing climate over Northeast Canada." Climate Dynamics 48, no. 9-10 (2016): 3227–46. http://dx.doi.org/10.1007/s00382-016-3260-y.

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22

Long, Z., W. Perrie, J. Gyakum, D. Caya, and R. Laprise. "Northern Lake Impacts on Local Seasonal Climate." Journal of Hydrometeorology 8, no. 4 (2007): 881–96. http://dx.doi.org/10.1175/jhm591.1.

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Abstract It is well known that large lakes can perturb local weather and climate through mesoscale circulations, for example, lake effects on storms and lake breezes, and the impacts on fluxes of heat, moisture, and momentum. However, for both large and small lakes, the importance of atmosphere–lake interactions in northern Canada is largely unknown. Here, the Canadian Regional Climate Model (CRCM) is used to simulate seasonal time scales for the Mackenzie River basin and northwest region of Canada, coupled to simulations of Great Bear and Great Slave Lakes using the Princeton Ocean Model (POM

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Xue, Pengfei, Jeremy S. Pal, Xinyu Ye, John D. Lenters, Chenfu Huang, and Philip Y. Chu. "Improving the Simulation of Large Lakes in Regional Climate Modeling: Two-Way Lake–Atmosphere Coupling with a 3D Hydrodynamic Model of the Great Lakes." Journal of Climate 30, no. 5 (2017): 1605–27. http://dx.doi.org/10.1175/jcli-d-16-0225.1.

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Abstract Accurate representations of lake–ice–atmosphere interactions in regional climate modeling remain one of the most critical and unresolved issues for understanding large-lake ecosystems and their watersheds. To date, the representation of the Great Lakes two-way interactions in regional climate models is achieved with one-dimensional (1D) lake models applied at the atmospheric model lake grid points distributed spatially across a 2D domain. While some progress has been made in refining 1D lake model processes, such models are fundamentally incapable of realistically resolving a number o

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Deng, Bin, Shoudong Liu, Wei Xiao, Wei Wang, Jiming Jin, and Xuhui Lee. "Evaluation of the CLM4 Lake Model at a Large and Shallow Freshwater Lake*." Journal of Hydrometeorology 14, no. 2 (2013): 636–49. http://dx.doi.org/10.1175/jhm-d-12-067.1.

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Abstract Models of lake physical processes provide the lower flux boundary conditions for numerical predictions of weather and climate in lake basins. So far, there have been few studies on evaluating lake model performance at the diurnal time scale and against flux observations. The goal of this paper is to evaluate the National Center for Atmospheric Research Community Land Model version 4–Lake, Ice, Snow and Sediment Simulator using the eddy covariance and water temperature data obtained at a subtropical freshwater lake, Lake Taihu, in China. Both observations and model simulations reveal t

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Thomas, Blaine C., and Jonathan E. Martin. "A Synoptic Climatology and Composite Analysis of the Alberta Clipper." Weather and Forecasting 22, no. 2 (2007): 315–33. http://dx.doi.org/10.1175/waf982.1.

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Abstract Surface and upper-air analyses from the ECMWF Tropical Ocean Global Atmosphere (TOGA) dataset are used to construct a climatology of 177 Alberta clippers over 15 boreal cold seasons (October–March) from 1986/87 to 2000/01. The Alberta clipper (hereafter simply clipper) occurs most frequently during December and January and substantially less frequently during October and March. These cyclones generally move southeastward from the lee of the Canadian Rockies toward or just north of Lake Superior before progressing eastward into southeastern Canada or the northeastern United States, wit

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26

Chatain, Audrey, Scot C. R. Rafkin, Alejandro Soto, Ricardo Hueso, and Aymeric Spiga. "Air–Sea Interactions on Titan: Effect of Radiative Transfer on the Lake Evaporation and Atmospheric Circulation." Planetary Science Journal 3, no. 10 (2022): 232. http://dx.doi.org/10.3847/psj/ac8d0b.

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Abstract Titan’s northern high latitudes host many large hydrocarbon lakes. Like water lakes on Earth, Titan’s lakes are constantly subject to evaporation. This process strongly affects the atmospheric methane abundance, the atmospheric temperature, the lake mixed layer temperature, and the local wind circulation. In this work we use a 2D atmospheric mesoscale model coupled to a slab lake model to investigate the effect of solar and infrared radiation on the exchange of energy and methane between Titan’s lakes and atmosphere. The magnitude of solar radiation reaching the surface of Titan throu

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Liu, Ximing, Hongbin Chen, Yanan Liu, Lujun Jiang, and Hongyan Chen. "Observational Study on Air-Water Interactions over Poyang Lake during a Cold Season." MAUSAM 75, no. 3 (2024): 715–28. http://dx.doi.org/10.54302/mausam.v75i3.5961.

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ABSTRACT In a lake, the heat and energy budgets and evaporation are the most fundamental components of the regional weather and climate and are controlled by the interactions between the lake and the atmosphere. Poyang Lake is the largest freshwater lake in China. The surface area of this shallow lake, located in the central and lower catchment of the Yangtze River, southeastern China, varies across the year based on the precipitation. A steel platform was built in the northeast open-water area of the lake to measure surface energy fluxes and other related atmospheric/hydrologic variables duri

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Xue, Pengfei, Chenfu Huang, Yafang Zhong, et al. "Enhancing winter climate simulations of the Great Lakes: insights from a new coupled lake–ice–atmosphere (CLIAv1) system on the importance of integrating 3D hydrodynamics with a regional climate model." Geoscientific Model Development 18, no. 13 (2025): 4293–316. https://doi.org/10.5194/gmd-18-4293-2025.

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Abstract. The Laurentian Great Lakes significantly influence the climate of the Midwest and Northeast United States due to their vast thermal inertia, moisture source potential, and complex heat and moisture flux dynamics. This study presents a newly developed coupled lake–ice–atmosphere (CLIAv1) modeling system for the Great Lakes by coupling the National Aeronautics and Space Administration (NASA) Unified Weather Research and Forecasting (NU-WRF) regional climate model (RCM) with the three-dimensional (3D) Finite Volume Community Ocean Model (FVCOM) and investigates the impact of coupled dyn

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Potes, M., R. Salgado, M. J. Costa, et al. "Lake–atmosphere interactions at Alqueva reservoir: a case study in the summer of 2014." Tellus A: Dynamic Meteorology and Oceanography 69, no. 1 (2017): 1272787. http://dx.doi.org/10.1080/16000870.2016.1272787.

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Şen, Z., M. Kadioğlu, and E. Batur. "Cluster regression model and level fluctuation features of Van Lake, Turkey." Annales Geophysicae 17, no. 2 (1999): 273–79. http://dx.doi.org/10.1007/s00585-999-0273-4.

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Abstract. Lake water levels change under the influences of natural and/or anthropogenic environmental conditions. Among these influences are the climate change, greenhouse effects and ozone layer depletions which are reflected in the hydrological cycle features over the lake drainage basins. Lake levels are among the most significant hydrological variables that are influenced by different atmospheric and environmental conditions. Consequently, lake level time series in many parts of the world include nonstationarity components such as shifts in the mean value, apparent or hidden periodicities.

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Potes, M., M. J. Costa, and R. Salgado. "Satellite remote sensing of water turbidity in Alqueva reservoir and implications on lake modelling." Hydrology and Earth System Sciences 16, no. 6 (2012): 1623–33. http://dx.doi.org/10.5194/hess-16-1623-2012.

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Abstract. The quality control and monitoring of surface freshwaters is crucial, since some of these water masses constitute essential renewable water resources for a variety of purposes. In addition, changes in the surface water composition may affect the physical properties of lake water, such as temperature, which in turn may impact the interactions of the water surface with the lower atmosphere. The use of satellite remote sensing to estimate the water turbidity of Alqueva reservoir, located in the south of Portugal, is explored. A validation study of the satellite derived water leaving spe

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Huziy, Oleksandr, Bernardo Teufel, Laxmi Sushama, and Ram Yerubandi. "Heavy Lake-Effect Snowfall Changes and Mechanisms for the Laurentian Great Lakes Region." Atmosphere 12, no. 12 (2021): 1577. http://dx.doi.org/10.3390/atmos12121577.

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Heavy lake-effect snowfall (HLES) events are snowfall events enhanced by interactions between lakes and overlying cold air. Significant snowfall rates and accumulations caused during such events disrupt socioeconomic activities and sometimes lead to lethal consequences. The aim of this study is to assess projected changes to HLES by the end of the century (2079–2100) using a regional climate model for the first time with 3D representation for the Laurentian Great Lakes. When compared to observations over the 1989–2010 period, the model is able to realistically reproduce key mechanisms and char

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Penenko, V. V., and E. A. Tsvetova. "Mathematical models for the study of interactions in the system lake baikal-atmosphere of the region." Journal of Applied Mechanics and Technical Physics 40, no. 2 (1999): 308–16. http://dx.doi.org/10.1007/bf02468528.

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Willeit, Matteo, and Andrey Ganopolski. "PALADYN v1.0, a comprehensive land surface–vegetation–carbon cycle model of intermediate complexity." Geoscientific Model Development 9, no. 10 (2016): 3817–57. http://dx.doi.org/10.5194/gmd-9-3817-2016.

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Abstract. PALADYN is presented; it is a new comprehensive and computationally efficient land surface–vegetation–carbon cycle model designed to be used in Earth system models of intermediate complexity for long-term simulations and paleoclimate studies. The model treats in a consistent manner the interaction between atmosphere, terrestrial vegetation and soil through the fluxes of energy, water and carbon. Energy, water and carbon are conserved. PALADYN explicitly treats permafrost, both in physical processes and as an important carbon pool. It distinguishes nine surface types: five different v

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Liston, Glen E., and Dorothy K. Hall. "An energy-balance model of lake-ice evolution." Journal of Glaciology 41, no. 138 (1995): 373–82. http://dx.doi.org/10.1017/s0022143000016245.

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AbstractA physically based mathematical model of the coupled lake, lake ice, snow and atmosphere system is developed for studying terrestrial-atmospheric interactions in high-elevation and high-latitude regions. The ability to model lake-ice freeze-up, break-up, total ice thickness and ice type offers the potential to describe the effects of climate change in these regions. Model output is validated against lake-ice observations made during the winter of 1992–93 in Glacier National Park, Montana. U.S.A. The model is driven with observed daily atmospheric forcing of precipitation, wind speed an

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Liston, Glen E., and Dorothy K. Hall. "An energy-balance model of lake-ice evolution." Journal of Glaciology 41, no. 138 (1995): 373–82. http://dx.doi.org/10.3189/s0022143000016245.

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AbstractA physically based mathematical model of the coupled lake, lake ice, snow and atmosphere system is developed for studying terrestrial-atmospheric interactions in high-elevation and high-latitude regions. The ability to model lake-ice freeze-up, break-up, total ice thickness and ice type offers the potential to describe the effects of climate change in these regions. Model output is validated against lake-ice observations made during the winter of 1992–93 in Glacier National Park, Montana. U.S.A. The model is driven with observed daily atmospheric forcing of precipitation, wind speed an

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Lockot, Gregori, Arne Ramisch, Bernd Wünnemann, et al. "A Process- and Provenance-Based Attempt to Unravel Inconsistent Radiocarbon Chronologies in Lake Sediments: An Example from Lake Heihai, North Tibetan Plateau (China)." Radiocarbon 57, no. 5 (2015): 1003–19. http://dx.doi.org/10.2458/azu_rc.57.18221.

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Aquatic macrophytes from a lacustrine environment are highly prone to a reservoir effect, resulting in an overestimation of age. This is often caused by the incorporation of dissolved carbon (CO2 and HCO3–) through photosynthesis from lake waters that have a different 14C activity than the atmosphere. The atmosphere-water disparity is often produced by a mixing of carbon between the water body and its terrestrial surroundings, a process highly prone to temporal variations. Thus, only a comprehensive understanding of the 14C budget over time enables a reliable chronology of lacustrine records.

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Durnford, D., V. Fortin, G. C. Smith, et al. "Toward an Operational Water Cycle Prediction System for the Great Lakes and St. Lawrence River." Bulletin of the American Meteorological Society 99, no. 3 (2018): 521–46. http://dx.doi.org/10.1175/bams-d-16-0155.1.

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Abstract In this time of a changing climate, it is important to know whether lake levels will rise, potentially causing flooding, or river flows will dry up during abnormally dry weather. The Great Lakes region is the largest freshwater lake system in the world. Moreover, agriculture, industry, commerce, and shipping are active in this densely populated region. Environment and Climate Change Canada (ECCC) recently implemented the Water Cycle Prediction System (WCPS) over the Great Lakes and St. Lawrence River watershed (WCPS-GLS version 1.0) following a decade of research and development. WCPS

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Huang, Wenfeng, Bin Cheng, Jinrong Zhang, et al. "Modeling experiments on seasonal lake ice mass and energy balance in the Qinghai–Tibet Plateau: a case study." Hydrology and Earth System Sciences 23, no. 4 (2019): 2173–86. http://dx.doi.org/10.5194/hess-23-2173-2019.

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Abstract. The lake-rich Qinghai–Tibet Plateau (QTP) has significant impacts on regional and global water cycles and monsoon systems through heat and water vapor exchange. The lake–atmosphere interactions have been quantified over open-water periods, yet little is known about the lake ice thermodynamics and heat and mass balance during the ice-covered season due to a lack of field data. In this study, a high-resolution thermodynamic ice model was applied in experiments of lake ice evolution and energy balance of a shallow lake in the QTP. Basal growth and melt dominated the seasonal evolution o

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Hansen, Sascha Hellmann, Inger Kappel Schmidt, and Klaus Steenberg Larsen. "Introducing LTER-DK and SITES Denmark - Infrastructure for long-term ecosystem research in Denmark." ARPHA Conference Abstracts 8 (May 28, 2025): e156302. https://doi.org/10.3897/aca.8.e156302.

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LTER-DK is a network of ten existing Danish platforms for long-term monitoring of ecosystems. In 2020, LTER-DK was accepted on the national Danish roadmap, and received funding for five years as the Danish node for eLTER RI in 2022. The Danish research platforms include terrestrial, freshwater, and coastal systems spread across the country. LTER-DK uses whole ecosystem approaches to observe and analyse the environmental system, with a focus on the interaction between biodiversity, biogeochemistry, hydrology and land-use. Several of the research platforms in LTER-DK are part of other networks,

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Wang, Binbin, Yaoming Ma, Yan Wang, et al. "Analysis of Lake Stratification and Mixing and Its Influencing Factors over High Elevation Large and Small Lakes on the Tibetan Plateau." Water 15, no. 11 (2023): 2094. http://dx.doi.org/10.3390/w15112094.

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Lake stratification and mixing processes can influence gas and energy transport in the water column and water–atmosphere interactions, thus impacting limnology and local climate. Featuring the largest high-elevation inland lake zone in the world, comprehensive and comparative studies on the evolution of lake stratification and mixing and their driving forces are still quite limited. Here, using valuable temperature chain measurements in four large lakes (Nam Co, Dagze Co, Bangong Co, and Paiku Co) and a “small lake” adjacent to Nam Co, our objectives are to investigate the seasonal and diurnal

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Zhang, Z. Q., G. P. Wang, X. G. Lv, H. J. Jia, and Q. H. Xu. "The sharp decline of East Asian summer monsoon at mid-Holocene indicated by the lake-wetland transition in the Sanjiang Plain, northeastern China." Climate of the Past Discussions 10, no. 6 (2014): 4595–622. http://dx.doi.org/10.5194/cpd-10-4595-2014.

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Abstract. The timing of the waxing and wining of the East Asian summer monsoon during the Holocene is still under debate. In present study, we present the high-resolution grain-size and LOI records from a well-dated mud/peat profile to reveal the lake-wetland transition in the Sanjiang Plain and discuss its significance to Holocene monsoon evolutions. The results show that the shallow-water lakes have developed in low-lying areas of the plain before 4600 yr BP, corresponding to the Holocene monsoon maximum. Thereafter, the wetlands began to initiate with the extinction of the paleolakes, marki

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Ma, Weiyao, Ling Bai, Weiqiang Ma, et al. "Interannual and Monthly Variability of Typical Inland Lakes on the Tibetan Plateau Located in Three Different Climatic Zones." Remote Sensing 14, no. 19 (2022): 5015. http://dx.doi.org/10.3390/rs14195015.

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Changes in lake water volume can reflect variations in regional hydrometeorology and are a sensitive indicator of regional environmental change. The Tibetan Plateau, referred to as the “Asian Water Tower”, has a large number of lakes. These lakes are in a natural state and are relatively unaffected by human activities. Understanding the changes to lake water volume is a key issue for the study of lake-atmosphere interactions and the effects of lake expansion and contraction on regional climate. By using multisource remote sensing and water level observations, this study systematically analyzed

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Wang, Binbin, Yaoming Ma, Yan Wang, Zhongbo Su, and Weiqiang Ma. "Significant differences exist in lake-atmosphere interactions and the evaporation rates of high-elevation small and large lakes." Journal of Hydrology 573 (June 2019): 220–34. http://dx.doi.org/10.1016/j.jhydrol.2019.03.066.

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Wen, Ruilin, Jule Xiao, Zhigang Chang, et al. "Holocene climate changes in the mid-high-latitude-monsoon margin reflected by the pollen record from Hulun Lake, northeastern Inner Mongolia." Quaternary Research 73, no. 2 (2010): 293–303. http://dx.doi.org/10.1016/j.yqres.2009.10.006.

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Pollen-assemblage data from a sediment core from Hulun Lake in northeastern Inner Mongolia describe the changes in the vegetation and climate of the East Asian monsoon margin during the Holocene. Dry steppe dominated the lake basin from ca. 11,000 to 8000 cal yr BP, suggesting a warm and dry climate. Grasses and birch forests expanded 8000 to 6400 cal yr BP, implying a remarkable increase in the monsoon precipitation. From 6400 to 4400 cal yr BP, the climate became cooler and drier. Chenopodiaceae dominated the interval from 4400 to 3350 cal yr BP, marking extremely dry condition. Artemisia re

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Prior, Elizabeth M., Gretchen R. Miller, and Kelly Brumbelow. "Topographic and Landcover Influence on Lower Atmospheric Profiles Measured by Small Unoccupied Aerial Systems (sUAS)." Drones 5, no. 3 (2021): 82. http://dx.doi.org/10.3390/drones5030082.

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Small unoccupied aerial systems (sUASs) are increasingly being used for field data collection and remote sensing purposes. Their ease of use, ability to carry sensors, low cost, and precise maneuverability and navigation make them a versatile tool for a field researcher. Procedures and instrumentation for sUASs are largely undefined, especially for atmospheric and hydrologic applications. The sUAS’s ability to collect atmospheric data for characterizing land–atmosphere interactions was examined at three distinct locations: Costa Rican rainforest, mountainous terrain in Georgia, USA, and land s

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Gerken, T., W. Babel, M. Herzog, et al. "High-resolution modelling of interactions between soil moisture and convection development in mountain enclosed Tibetan basin." Hydrology and Earth System Sciences Discussions 12, no. 5 (2015): 4631–75. http://dx.doi.org/10.5194/hessd-12-4631-2015.

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Abstract. The Tibetan Plateau plays a significant role in the atmospheric circulation and the Asian monsoon system. Turbulent surface fluxes and the evolution of boundary layer clouds to deep and moist convection provide a feedback system that modifies the Plateau's surface energy balance on scales that are currently unresolved in mesoscale models. This work analyses the land surface's role and specifically the influence of soil moisture on the triggering of convection at a cross-section of the Nam Co Lake basin, 150 km north of Lhasa using a cloud resolving atmospheric model with a fully coup

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Grenfell, Thomas C., Donald K. Perovich, Hajo Eicken, et al. "Energy- and mass-balance observations of the land–ice–ocean–atmosphere system near Barrow, Alaska, USA, November 1999–July 2002." Annals of Glaciology 44 (2006): 193–99. http://dx.doi.org/10.3189/172756406781811222.

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AbstractWe present results from a comprehensive field study carried out near Barrow, Alaska, USA, designed to characterize local- to intermediate-scale sea-ice processes in the Arctic coastal zone of central importance to the annual cycle and evolution of the coastal sea ice. Included in this are the behavior of the snow cover of the ice and adjacent tundra and lake system; concurrent studies of mass balance of the sea ice and lake ice; interaction of shortwave radiation with the shore-fast ice and the adjacent land surfaces; evolution of the area coverage and distribution of the various surfa

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Gerken, T., W. Babel, M. Herzog, et al. "High-resolution modelling of interactions between soil moisture and convective development in a mountain enclosed Tibetan Basin." Hydrology and Earth System Sciences 19, no. 9 (2015): 4023–40. http://dx.doi.org/10.5194/hess-19-4023-2015.

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Abstract. The Tibetan Plateau plays a significant role in atmospheric circulation and the Asian monsoon system. Turbulent surface fluxes and the evolution of boundary-layer clouds to deep and moist convection provide a feedback system that modifies the plateau's surface energy balance on scales that are currently unresolved in mesoscale models. This work analyses the land surface's role and specifically the influence of soil moisture on the triggering of convection at a cross section of the Nam Co Lake basin, 150 km north of Lhasa using a cloud-resolving atmospheric model with a fully coupled

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Newby, Paige E., Bryan N. Shuman, Jeffrey P. Donnelly, and Dana MacDonald. "Repeated century-scale droughts over the past 13,000 yr near the Hudson River watershed, USA." Quaternary Research 75, no. 3 (2011): 523–30. http://dx.doi.org/10.1016/j.yqres.2011.01.006.

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AbstractLong-term sediment and ground-penetrating radar data from Davis Pond, a small lake near the Hudson River valley, reveal past droughts in a historically humid region that presently supplies water to millions of people in and around New York City. A minimum of eleven sandy paleoshoreline deposits in the lake date from 13.4 to 0.6 cal ka BP. The deposits span 1500 to 200 yr between bracketing radiocarbon ages, and intrude into lacustrine silts up to 9.0 m below the modern lake surface in a transect of six sediment cores. Three low stands, ca. 13.4–10.9, 9.2 and 8.2 cal ka BP indicate low

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