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Gotowe bibliografie tematyczne / Terrestrial ice loss

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Gotowa bibliografia na temat „Terrestrial ice loss”

Autor: Grafiati

Data publikacji: 2 czerwca 2025

Data aktualizacji: 31 lipca 2025

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Artykuły w czasopismach na temat "Terrestrial ice loss"

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Spada, G., J. L. Bamber, and R. T. W. L. Hurkmans. "The gravitationally consistent sea-level fingerprint of future terrestrial ice loss." Geophysical Research Letters 40, no. 3 (2013): 482–86. https://doi.org/10.5281/zenodo.6996.

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We solve the sea-level equation to investigate the pattern of the gravitationally self-consistent sea-level variations (fingerprints) corresponding to modeled scenarios of future terrestrial ice melt. These were obtained from separate ice dynamics and surface mass balance models for the Greenland and Antarctic ice sheets and by a regionalized mass balance model for glaciers and ice caps. For our mid-range scenario, the ice melt component of total sea-level change attains its largest amplitude in the equatorial oceans, where we predict a cumulative sea-level rise of ~ 25 cm and rates of change

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Spada, G., J. L. Bamber, and R. T. W. L. Hurkmans. "The gravitationally consistent sea-level fingerprint of future terrestrial ice loss." Geophysical Research Letters 40, no. 3 (2013): 482–86. http://dx.doi.org/10.1029/2012gl053000.

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Tsuji, Masaharu, Warwick F. Vincent, Yukiko Tanabe, and Masaki Uchida. "Glacier Retreat Results in Loss of Fungal Diversity." Sustainability 14, no. 3 (2022): 1617. http://dx.doi.org/10.3390/su14031617.

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Walker Glacier near the northern coast of Ellesmere Island in the Canadian High Arctic (terrestrial margin of the ‘Last Ice Area’) is undergoing rapid ice attrition in response to climate change. We applied culture and molecular methods to investigate fungal diversity at the terminus of this glacier. Analysis of the mycoflora composition showed that the Walker Glacier isolates separated into two clusters: the surface of the glacier ice and the glacier foreland. The recently exposed sediments of the foreland had a lower fungal diversity and different species from those on the ice, with the exce

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Brun, Fanny, Patrick Wagnon, Etienne Berthier, et al. "Ice cliff contribution to the tongue-wide ablation of Changri Nup Glacier, Nepal, central Himalaya." Cryosphere 12, no. 11 (2018): 3439–57. http://dx.doi.org/10.5194/tc-12-3439-2018.

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Abstract. Ice cliff backwasting on debris-covered glaciers is recognized as an important mass-loss process that is potentially responsible for the “debris-cover anomaly”, i.e. the fact that debris-covered and debris-free glacier tongues appear to have similar thinning rates in the Himalaya. In this study, we quantify the total contribution of ice cliff backwasting to the net ablation of the tongue of Changri Nup Glacier, Nepal, between 2015 and 2017. Detailed backwasting and surface thinning rates were obtained from terrestrial photogrammetry collected in November 2015 and 2016, unmanned air v

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Jenkins, Deborah A., Nicolas Lecomte, James A. Schaefer, et al. "Loss of connectivity among island-dwelling Peary caribou following sea ice decline." Biology Letters 12, no. 9 (2016): 20160235. http://dx.doi.org/10.1098/rsbl.2016.0235.

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Global warming threatens to reduce population connectivity for terrestrial wildlife through significant and rapid changes to sea ice. Using genetic fingerprinting, we contrasted extant connectivity in island-dwelling Peary caribou in northern Canada with continental-migratory caribou. We next examined if sea-ice contractions in the last decades modulated population connectivity and explored the possible impact of future climate change on long-term connectivity among island caribou. We found a strong correlation between genetic and geodesic distances for both continental and Peary caribou, even

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Bargagli, R. "Terrestrial ecosystems of the Antarctic Peninsula and their responses to climate change and anthropogenic impacts." Ukrainian Antarctic Journal, no. 2 (December 2020): 84–97. http://dx.doi.org/10.33275/1727-7485.2.2020.656.

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Antarctica and the Southern Ocean are unique natural laboratories where organisms adapted to extreme environmental conditions have evolved in isolation for millions of years. These unique biotic communities on Earth are facing complex climatic and environmental changes. Terrestrial ecosystems in the Antarctic Peninsula Region (APR) have experienced the highest rate of climate warming and, being the most impacted by human activities, are facing the greatest risk of detrimental changes. This review provides an overview of the most recent findings on how biotic communities in terrestrial ecosyste

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BRUN, FANNY, PASCAL BURI, EVAN S. MILES, et al. "Quantifying volume loss from ice cliffs on debris-covered glaciers using high-resolution terrestrial and aerial photogrammetry." Journal of Glaciology 62, no. 234 (2016): 684–95. http://dx.doi.org/10.1017/jog.2016.54.

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ABSTRACTMass losses originating from supraglacial ice cliffs at the lower tongues of debris-covered glaciers are a potentially large component of the mass balance, but have rarely been quantified. In this study, we develop a method to estimate ice cliff volume losses based on high-resolution topographic data derived from terrestrial and aerial photogrammetry. We apply our method to six cliffs monitored in May and October 2013 and 2014 using four different topographic datasets collected over the debris-covered Lirung Glacier of the Nepalese Himalayas. During the monsoon, the cliff mean backwast

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Walter, Andrea, Martin P. Lüthi, and Andreas Vieli. "Calving event size measurements and statistics of Eqip Sermia, Greenland, from terrestrial radar interferometry." Cryosphere 14, no. 3 (2020): 1051–66. http://dx.doi.org/10.5194/tc-14-1051-2020.

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Abstract. Calving is a crucial process for the recently observed dynamic mass loss changes of the Greenland ice sheet. Despite its importance for global sea level change, major limitations in understanding the process of calving remain. This study presents high-resolution calving event data and statistics recorded with a terrestrial radar interferometer at the front of Eqip Sermia, a marine-terminating outlet glacier in Greenland. The derived digital elevation models with a spatial resolution of several metres recorded at 1 min intervals were processed to provide source areas and volumes of 90

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Wieber, Corina, Lasse Z. Jensen, Leendert Vergeynst, et al. "Terrestrial runoff is an important source of biological ice-nucleating particles in Arctic marine systems." Atmospheric Chemistry and Physics 25, no. 6 (2025): 3327–46. https://doi.org/10.5194/acp-25-3327-2025.

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Abstract. The accelerated warming of the Arctic manifests in sea ice loss and melting glaciers, significantly altering the dynamics of marine biota. This disruption in marine ecosystems can lead to an increased emission of biological ice-nucleating particles (INPs) from the ocean into the atmosphere. Once airborne, these INPs induce cloud droplet freezing, thereby affecting cloud lifetime and radiative properties. Despite the potential atmospheric impacts of marine INPs, their properties and sources remain poorly understood. By analyzing sea bulk water and the sea surface microlayer in two sou

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Cuzzone, Joshua K., Nicolás E. Young, Mathieu Morlighem, Jason P. Briner, and Nicole-Jeanne Schlegel. "Simulating the Holocene deglaciation across a marine-terminating portion of southwestern Greenland in response to marine and atmospheric forcings." Cryosphere 16, no. 6 (2022): 2355–72. http://dx.doi.org/10.5194/tc-16-2355-2022.

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Abstract. Numerical simulations of the Greenland Ice Sheet (GrIS) over geologic timescales can greatly improve our knowledge of the critical factors driving GrIS demise during climatically warm periods, which has clear relevance for better predicting GrIS behavior over the upcoming centuries. To assess the fidelity of these modeling efforts, however, observational constraints of past ice sheet change are needed. Across southwestern Greenland, geologic records detail Holocene ice retreat across both terrestrial-based and marine-terminating environments, providing an ideal opportunity to rigorou

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Części książek na temat "Terrestrial ice loss"

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Zlotnicki, Victor, Srinivas Bettadpur, Felix W. Landerer, and Michael M. Watkins. "Gravity Recovery and Climate Experiment (GRACE) gravity recovery and climate experiment (GRACE) : Detection of Ice Mass Loss ice ice mass loss , Terrestrial Mass Changes terrestrial mass changes , and Ocean Mass Gains ocean/oceanic mass gains." In Encyclopedia of Sustainability Science and Technology. Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4419-0851-3_745.

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Zlotnicki, Victor, Srinivas Bettadpur, Felix W. Landerer, and Michael M. Watkins. "Gravity Recovery and Climate Experiment (GRACE): Detection of Ice Mass Loss, Terrestrial Mass Changes, and Ocean Mass Gains." In Earth System Monitoring. Springer New York, 2012. http://dx.doi.org/10.1007/978-1-4614-5684-1_7.

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Howarth, Brigitte. "Terrestrial Arthropod Diversity in the United Arab Emirates." In A Natural History of the Emirates. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-37397-8_17.

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AbstractDespite harsh climatic conditions and low and erratic rainfall patterns, the United Arab Emirates’ (UAE) terrestrial arthropod fauna is diverse and extremely well adapted to the local environment, with some species occurring in high abundance. Until recently, the UAE’s terrestrial arthropods were poorly studied. The past two decades have seen the knowledge of arthropod diversity increase dramatically, with more than 4000 species now known to occur in the Emirates, including hundreds of species that were previously unknown for the UAE and had never been recorded globally. With so many s

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Hinkel, Kenneth M., and Andrew W. Ellis. "Cryosphere." In Geography in America at the Dawn of the 21st Century. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780198233923.003.0013.

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The cryosphere refers to the Earth’s frozen realm. As such, it includes the 10 percent of the terrestrial surface covered by ice sheets and glaciers, an additional 14 percent characterized by permafrost and/or periglacial processes, and those regions affected by ephemeral and permanent snow cover and sea ice. Although glaciers and permafrost are confined to high latitudes or altitudes, areas seasonally affected by snow cover and sea ice occupy a large portion of Earth’s surface area and have strong spatiotemporal characteristics. Considerable scientific attention has focused on the cryosphere

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Fleming, James R. "Global Warming? The Early Twentieth Century." In Historical Perspectives on Climate Change. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195078701.003.0014.

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In the first half of the twentieth century, most scientists did not believe that increased CO2 levels would result in global warming. It was thought that at current atmospheric concentrations, the gas already absorbed all the available long-wave radiation; thus any increases in CO2 would not change the radiative heat balance of the planet but might augment plant growth. Other mechanisms of climatic change, although highly speculative, were given more credence, especially changes in solar luminosity, atmospheric transparency, and the Earth’s orbital elements. By the 1950s, as temperatures aroun

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Harvey Pough, F., Robin M. Andrews, Martha L. Crump, Alan H. Savitzky, Kentwood D. Wells, and Matthew C. Brandley. "Water and Temperature Relations." In Herpetology. Oxford University Press, 2015. http://dx.doi.org/10.1093/hesc/9781605352336.003.0008.

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This chapter assesses biophysical ecology, which is the study of how animals exchange heat and water with their environments. Reptiles and amphibians have been especially important in the development of this field because interaction with the physical environment is such a conspicuous part of their lives. Regulating the amount of water in the body requires balancing gain and loss. In a steady state (i.e. no change in body water content), the total intake of water must equal the total water loss, and each side of the water-balance equation has several components. This is a general equation that

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Piantadosi, Claude A. "Water That Makes Men Mad." In The Biology of Human Survival. Oxford University PressNew York, NY, 2003. http://dx.doi.org/10.1093/oso/9780195165012.003.0006.

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Abstract When Samuel Taylor Coleridge wrote the words, “Water, water everywhere, but not a drop to drink” in The Rime of the Ancient Mariner in 1798, the dangers of drinking seawater had been known for thousands of years. Seawater does indeed make men mad. Historical evidence indicates the ancient Egyptians knew seawater was not potable, but the earliest realization that it was unsafe to drink has been lost to antiquity. In pre-Columbian times the greatest fear of venturing too far from land on the ocean was not falling off the surface of the Earth but lack of fresh drinking water. From a huma

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Mondal, Abhishek, Deepak Mishra, Ganesh Prasad, and Ashraf Hossain. "Optimal Unmanned Aerial Vehicle Control and Designs for Load Balancing in Intelligent Wireless Communication Systems." In Edge Computing - Technology, Management and Integration [Working Title]. IntechOpen, 2023. http://dx.doi.org/10.5772/intechopen.110312.

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Maintaining reliable wireless connectivity is essential for the continuing growth of mobile devices and their massive access to the Internet of Things (IoT). However, terrestrial cellular networks often fail to meet their required quality of service (QoS) demand because of the limited spectrum capacity. Although the deployment of more base stations (BSs) in a concerned area is costly and requires regular maintenance. Alternatively, unmanned aerial vehicles (UAVs) could be a potential solution due to their ability of on-demand coverage and the high likelihood of strong line-of-sight (LoS) commu

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Ehlers, Jürgen. "Quaternary Climatic Changes and Landscape Evolution." In The Physical Geography of Western Europe. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199277759.003.0012.

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The last 2–3 Ma have witnessed climatic changes of a scale unknown to the preceding 300 Ma. In the cold periods vegetation was reduced to a steppe, giving rise to large-scale aeolian deposition of sand and loess and river sands and gravels. In the warm stages, flora and fauna recolonized the region. Parts of Europe were repeatedly covered by mountain glaciers or continental ice sheets which brought along huge amounts of unweathered rock debris from their source areas. The ice sheets dammed rivers and redirected drainage towards the North Sea. They created a new, glacial landscape. This chapter

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Streszczenia konferencji na temat "Terrestrial ice loss"

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Emmons, E. B., and G. Walton. "A Review of Cluster Filtering Methods for Point-Cloud-Based Rockfall Monitoring." In 58th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2024. http://dx.doi.org/10.56952/arma-2024-0580.

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ABSTRACT: The standard methodology for through-time rockfall analysis from slope point clouds consists of computing changes between lidar scans, followed by grouping areas of significant change using unsupervised clustering (e.g., DBSCAN). Clusters found are indicative of a potential rockfall and can be used for the construction of a comprehensive rockfall database. However, clustered change not representing true rockfalls is common, often accounting for the majority of identified objects. Identifying these erroneous clusters requires hours of manual verification; therefore, the search for an

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Raporty organizacyjne na temat "Terrestrial ice loss"

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Thomas, Douglas, and Mellon Michael. Sublimation of terrestrial permafrost and the implications for ice-loss processes on Mars. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41244.

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Sublimation of ice is rate-controlled by vapor transport away from its outer surface and may have generated landforms on Mars. In ice-cemented ground (permafrost), the lag of soil particles remaining after ice loss decreases subsequent sublimation. Varying soil-ice ratios lead to differential lag development. Here we report 52 years of sublimation measurements from a permafrost tunnel near Fairbanks, Alaska, and constrain models of sublimation, diffusion through porous soil, and lag formation. We derive the first long-term in situ effective diffusion coefficient of ice-free loess, a Mars analo

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Gaskin, Tosin, Matthew Balazik, Catherine Thomas, et al. Living shoreline in USACE projects : a review. Engineer Research and Development Center (U.S.), 2025. https://doi.org/10.21079/11681/49678.

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The term living shoreline (LS) refers to the practice of shoreline stabilization using natural elements (e.g., vegetation, oysters, logs, etc.) in a way that maintains continuity and connectivity between terrestrial and aquatic habitats. This report provides a review of LS practices to assess the applicability of these engineering techniques for US Army Corps of Engineers (USACE) projects. Specifically, this review examines the current state of knowledge regarding LS efforts through evaluation of peer-reviewed literature, agency reports, web tools, applications, and relevant guidance. It is im

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Schuurman, Gregor, and David Lawrence. Adapting to climate change-driven loss of ecologically important species and processes from park ecosystems: A study of management options for Glacier National Park streams in the context of National Park Service policy and guidance. National Park Service, 2025. https://doi.org/10.36967/2307053.

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The traditional paradigm in mainstream environmental stewardship assumes a stationary climate in which climatic and ecological change generally occur within bounds (e.g., “natural range of variability”) and managers can conserve ecosystems by preserving their historically co-occurring species, natural communities, and physical and biological processes. For example, 2006 Management Policies, the current NPS management policies document, suggests that by preserving ecosystem components and processes in their natural condition, the NPS will prevent resource degradation and thus avoid any subseque

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Rich, Megan, Charles Beightol, Christy Visaggi, Justin Tweet, and Vincent Santucci. Vicksburg National Military Park: Paleontological resource inventory (sensitive version). National Park Service, 2023. http://dx.doi.org/10.36967/2297321.

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Vicksburg National Military Park (VICK) was established for its historical significance as a one of the principle military sieges resulting in a turning point during the American Civil War. The steep terrain around the city of Vicksburg was integral in the military siege, providing high vantage points and a substrate that was easy to entrench for the armies, but unknown to many is the fossil content, particularly a diversity of fossil mollusks. These fossils at VICK are important paleontological resources which have yet to receive focused attention from park staff, visitors, and researchers. T

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