scispace - formally typeset
Search or ask a question

Effect glacier melting Antarctica vs Artic? 


Best insight from top research papers

Glacier melting in Antarctica and the Arctic has significant effects on the surrounding environment. In Antarctica, the melting of glacial ice below the sea surface and in regions with ice shelves and icebergs can impact the chemistry and biology of the Antarctic Surface Water (AASW) . The melting of glaciers in the Western Antarctic Peninsula and its surrounding islands influences biogeochemical processes in the water column and marine sediment, affecting nutrient fluxes and productivity in the Southern Ocean . The melting of the Greenland and Antarctic ice sheets also has implications for climate change. Meltwater from Greenland drives atmospheric cooling, sea-ice expansion, and changes in ocean circulation, while Antarctic meltwater affects the formation of Antarctic Bottom Water and the subsurface ocean around Antarctica . Additionally, the melting of glaciers and ice sheets contributes to rising sea levels, leading to coastal erosion, flooding, and habitat loss . The presence of sediment on glacier surfaces in Antarctica can also impact meltwater generation and delivery, affecting the timing and magnitude of ablation .

Answers from top 5 papers

More filters
Papers (5)Insight
The provided paper does not compare the effects of glacier melting in Antarctica and the Arctic.
The paper does not provide specific information about the effects of glacier melting in Antarctica versus the Arctic. The paper primarily focuses on the overall impact of glacier melting on sea levels and coastal habitats.
The paper states that both Greenland and Antarctic ice sheet melting lead to atmospheric cooling, sea-ice expansion, and changes in ocean circulation. However, it suggests that Antarctic meltwater will become a major driver of climate change, dominating that of Greenland meltwater in the future.
Copilot couldn't generate the response. Please try again after some time.
The provided paper specifically focuses on the effect of glacial ice melting on the Antarctic Surface Water (AASW). It does not provide information about the effect of glacier melting in the Arctic.

Related Questions

What is the relationship between the melting rate and the area of the glacier?5 answersThe relationship between the melting rate and the area of the glacier is influenced by various factors. Studies have shown that there is a power-law relation between glacier area and volume, with an exponent γ≈ 1.36. This means that as the area of the glacier decreases, the volume of melt also decreases. Additionally, the distribution of debris thickness on the glacier surface can induce differential melting, leading to variations in the melting rate. The thickness of debris cover is generally thicker in the lower reaches of the glacier and decreases with increasing distance from the snout. Furthermore, the volume-length scaling relations can be used to estimate changing glacier terminus and update glacier area changes, which can affect the melting rate. Overall, the relationship between melting rate and glacier area is complex and can be influenced by factors such as debris cover and glacier shape.
Whats the effect of the ice caps melting5 answersThe melting ice caps have various effects on the Earth's ecosystem and human civilization. The melting ice caps lead to rising sea levels, uncertain floods, and fluctuating seawater temperature, resulting in different storms like tornadoes and cyclones. The decline in the number of glaciers in the Antarctic Peninsula and the Arctic region affects the harmony of biodiversity. The melting ice caps also contribute to climate change, which creates difficulties for the food chain, habitats, and the economy. Additionally, the melting ice caps have commercial implications, as they open up the Northern Sea Route for high volume commercial traffic, reducing shipping distances and transportation days between Asia and Europe. This redirection of trade has major geopolitical implications and highlights the environmental pressure on the Arctic.
What is causing glacier melting in antartica?5 answersGlacier melting in Antarctica is caused by a combination of factors. Increased temperatures have led to faster melt in the glaciers of the Antarctic Peninsula. The ice shelf buttressing Antarctica's Pine Island Glacier has been melting rapidly due to a stronger circulation below the ice shelf. Additionally, black carbon emissions produced by fires in the Amazon have been found to cause glaciers in the Andes to absorb more sunlight and melt more. It is important to note that changes in precipitation are unlikely to offset the increased melt from warming. The COVID-19 pandemic may have also had an impact on the glacier melting rate, potentially slowing it down by 20% in the 2020-2021 period.
What mircroplastics affect glacier melting?4 answersMicroplastics have not been specifically mentioned in the provided abstracts. Therefore, there is no information available in these abstracts regarding the specific microplastics that affect glacier melting.
How do microplastics affect the melting of glaciers in Antarctica?5 answersMicroplastics have the potential to affect the melting of glaciers in Antarctica. They can contribute to the melting and rheological behavior of glaciers, which in turn influences the future meltwater contribution to the oceans and rising sea levels. Additionally, microplastics may have an impact on the snow/ice surface albedos in cryospheric regions, potentially enhancing cryospheric melting under rapid global warming and increasing plastic pollutants. The presence of microplastic particles in water, sediments, and biota around Antarctica indicates their widespread distribution and potential risk to the environment. The transport and accumulation of microplastics in bays near Antarctic research stations can be influenced by the characteristics of vertical migration and flow conditions, as well as the release time of wastewater during the tidal cycle. Overall, the presence of microplastics in Antarctica and their interactions with glaciers and the surrounding environment highlight the need for further research and improved wastewater treatment to mitigate their accumulation and potential impacts.
Is there a lake in chile that has influence from a glacier thats melting?5 answersYes, there is a lake in Chile that is influenced by a melting glacier. The research team found that a glacial lake in the Chileno Valley had unleashed a glacial lake outburst flood, causing devastation in the area. As mountain glaciers retreat in a warming climate, meltwater lakes can burst through unstable barriers, leading to flooding and destruction. Additionally, the study found that the rapid melting of glaciers has caused a decrease in temperature in the lakes, especially at deeper levels. This indicates that the melting glaciers are impacting the temperature of the lakes. Therefore, the melting glaciers in Chile are not only causing flooding but also influencing the temperature of the lakes in the region.

See what other people are reading

How has climate change influenced the melting of polar ice caps and glaciers?
5 answers
Climate change has significantly impacted the melting of polar ice caps and glaciers. The accelerated glacier wastage globally, attributed to climatic warming, has led to negative mass balances dominated by surface melt. In the Arctic, the Greenland Ice Sheet has experienced notable melt records, while other regions like Svalbard have shown less influence. Studies have shown that the majority of Arctic glaciers were smaller or absent during warmer periods in the early and middle Holocene, indicating a long-term trend of glacier fluctuations in response to changing temperatures. Additionally, surface melting in Antarctica has led to the formation of melt ponds and supraglacial lakes, impacting ice shelf stability and velocity, highlighting the critical role of surface melt in driving ice flow and destabilization. Continuous monitoring of these regions is crucial to assess the ongoing impact of climate change on polar ice masses.
How much did alpine glaciers decline compared to the pre-industrial time?
4 answers
Alpine glaciers have experienced significant decline compared to pre-industrial times. Studies indicate that glaciers in the European Alps began retreating from their mid-19th century maximum, marking the end of the Little Ice Age. The retreat has been attributed to factors like radiative forcing from industrial black carbon deposition on snow, leading to accelerated melting rates. Specifically, between 2000 and 2014, the entire European Alps saw a mass loss of 13 ± 0.2 Gt per year, with rapid glacier retreat averaging at -39 km² per year. Furthermore, simulations suggest that by 1930, the negative mass balances of Alpine glaciers reached around -30 m water equivalent, aligning with observed retreat patterns.
What are challanges faced by skiing athletes due to decrease in snow cover?
4 answers
Skiing athletes face challenges due to decreased snow cover caused by climate change. The impact of reduced snow cover affects the experiences of skiers and poses risks to the sport. Ski resorts have implemented measures like snow farming and artificial snow production to adapt to diminishing natural snowfall. However, projections suggest that many ski resorts may struggle to maintain adequate snow cover, leading to potential economic shifts towards summer activities and property development. Climate change threatens winter sports like skiing, snowboarding, and cross-country skiing, impacting mountain tourism and potentially concentrating winter sport activities in higher altitudes. These challenges highlight the urgent need for sustainable practices and adaptation strategies in the skiing industry to mitigate the effects of climate change on snow-dependent sports.
What is the effect of glacier orientation on melting?
5 answers
Glacier orientation plays a crucial role in the melting process. The distribution and significance of melting vary with elevation and exposure. Additionally, the effect of digital elevation model (DEM) resolution on glacier melt modeling shows that localized spatio-temporal variations in simulated melt are influenced by the representation of terrain morphology, affecting the grid cell-level hydrological balance. The Himalayan and Tibet Glaciers face accelerated melting due to climate change, with varying rates of retreat and terminus changes across the region. Furthermore, the effect of uniaxial orientation on the melting of polypropylene is attributed to the increase in configurational entropy of the extended melt, shifting the melting point to higher temperatures. Thus, glacier orientation impacts melting rates through complex interactions with terrain features and climatic conditions.
Does an increase in the surface-to-volume ratio of glaciers correlates with an accelerated rate of melting.?
5 answers
An increase in the surface-to-volume ratio of glaciers can indeed correlate with an accelerated rate of melting. The surface meltwater supply to the ice-sheet bed can lubricate ice flow, potentially leading to glacial acceleration. This mechanism is observed in Greenland, where surface meltwater reaching the bed enhances glacier speed, increasing ice flux into the ablation area and accelerating mass loss. Similarly, on the Antarctic Peninsula, drainage of surface meltwater to the bed triggers rapid ice flow accelerations in response to atmospheric warming, indicating a direct link between surface melting and glacier dynamics. Therefore, changes in the surface-to-volume ratio of glaciers can impact the rate of melting by influencing basal motion and ice flow dynamics, especially under warming climate conditions.
What are the primary factors that influence the phenology of landfast ice in various regions?
5 answers
The primary factors influencing the phenology of landfast ice in various regions include air temperature, solar radiation, wind speed, lake heat storage, snowfall, and local climatic variables. These factors play a crucial role in determining the freezing and breakup dates of landfast ice. Analytic models highlight the importance of air temperature and solar radiation in dictating freezing and breakup dates, with rates of change being significant. Additionally, the formation and breakup of landfast ice are influenced by the grounding of thick ice ridges, which provide lateral stability to the ice cover. Changes in ice phenology are linked to continental-scale variations in air temperature but are also impacted by localized climatic variables, emphasizing the need to consider both regional and local factors for accurate assessments.
How does ice shelf melting influence sea ice?
5 answers
Ice shelf melting significantly impacts sea ice dynamics. Basal ice shelf melting contributes to sea-level rise by reducing ice shelf buttressing, leading to increased ice discharge into the ocean. Additionally, the presence of fast ice plays a crucial role in modulating ice shelf melt rates, with a representation of fast ice dampening the melt rate increase over the 21st century. Furthermore, the formation of sea ice ponds due to meltwater runoff from ice shelves can decrease sea ice albedo, thinning it and potentially promoting instability by the ice shelf front. These interactions between ice shelf melting, fast ice presence, and sea ice dynamics underscore the complex relationship between Antarctic ice shelves and sea ice properties, highlighting the importance of considering these factors in understanding the broader impacts of climate change on polar regions.
When were geodetic observations of the movement of glaciers started?
5 answers
Geodetic observations of glacier movement began in the late 1950s at various glaciers in North America, including South Cascade Glacier, WA in 1958, Gulkana and Wolverine glaciers, AK in 1966, and later Sperry Glacier, MT in 2005. These observations have expanded globally, with a new approach combining glacier outlines from the Randolph Glacier Inventory and mass balance data from the Fluctuation of Glaciers database, allowing for a near-complete dataset of geodetic mass balance between 2000 and 2020. Additionally, precise observations of glacial movement using GPS and satellite images have been conducted, such as monitoring the Perito Moreno glacier in Patagonia, Argentina over the past five years. These observations play a crucial role in understanding the impact of global warming on glaciers.
How does a wind from continent to sea suspend sediments in the shelf?
5 answers
A wind blowing from the continent to the sea can suspend sediments in the shelf by enhancing turbulence and vertical mixing, leading to increased Sediment Suspended Concentrations (SSCs). This wind-induced turbulence intensifies the vertical mixing coefficient, crucial for suspended sediment modeling, especially with stronger winds. Additionally, the wind contributes significantly to the enlargement of SSCs above the High Concentration Layers (HCL) by transporting more sediment suspensions upward, particularly for finer sediments that are easier to suspend. Furthermore, the presence of island trapped waves generated by local wind forcing can induce significant sediment resuspension along the shelf, highlighting the coupling between atmospheric and shelf circulation as a mechanism for sediment dynamics. Overall, the wind's impact on sediment suspension is a complex interplay of turbulence, mixing, and wave interactions in coastal systems.
What is the science behind puddles?
5 answers
Puddles are formed due to internal melting of sea ice, caused by the absorption of solar radiation. Classical fluid theory struggles to explain puddle behavior, but a new theory incorporating intermolecular forces resolves this issue. In a laboratory model, sequential stages of an ombrophilic cyano-bacterial community formation on clay in a puddle were observed, showing the development of a complex structure. Puddles are not just water bodies; they play a crucial role in children's learning and development, offering unique sensory experiences that enhance their understanding of the world around them. Furthermore, sensitive imaging methods have confirmed the existence of electron and hole 'puddles' in graphene sheets, aligning with theoretical predictions. Overall, puddles exhibit diverse scientific phenomena, from physical processes to biological interactions and educational benefits.
How the snow cover is changed in himalayas?
5 answers
Snow cover in the Himalayas has shown significant changes over recent years. Studies in the Hindu Kush Himalayan (HKH) region and the Parvati River basin (PRB) indicate a decline in snow cover at higher altitudes, with major decreases observed between 4000–4500 and 5500–6000 m altitudes. Additionally, the Upper Ganga river basin has experienced reductions in snow melt runoff and glacier areas, with noticeable changes in runoff components. In the Bhagirathi River Basin (BRB), an increase in snow cover area (SCA) was noted, correlating with higher precipitation and Terrestrial Water Storage (TWS) over the basin. Climate change projections suggest a decrease in SCA at higher altitudes in the Himalayas, impacting river flow despite increased precipitation, highlighting the complex interplay between snow cover changes and climate variables in the region.