Black Carbon and Light-absorbing impurities in the Antarctic Peninsula

Author(s):  
Raul Cordero ◽  
Alessandro Damiani ◽  
Sarah Feron ◽  
Alia Khan ◽  
Jose Jorquera ◽  
...  

<p>Assessing the albedo response due to light-absorbing impurities (LAI) in coastal snowpacks has become of great interest in the light of the ‘Antarctic greening’. Reductions in the albedo (triggered by a change in air temperature or by the LAI deposition) can also enhance feedback mechanisms; as the albedo drops, the fraction of absorbed solar energy increases, which leads to additional albedo drops.</p><p>Here we assess the presence of Black Carbon (BC) and LAI in coastal snowpacks in the Antarctic Peninsula. The BC-equivalent contentwas assessed by applying the meltwater filtration (MF) technique to snow samples taken at 7 locations in theAntarctic Peninsula, from latitude 62<sup>o</sup>S to latitude 67<sup>o</sup>S. BC-equivalentconcentrations exhibited significant geographical differences,but were found to be generally lower than 5 ng/g (in the range of those reported for the Arctic Ocean and Greenland). Moreover, the Angstrom coefficients were found to be particularly high at the northern tip of the Antarctic Peninsula,likely due to the snow algae presence. After the onset of melt, red snow algae bloom, significantly affecting the surface albedo, as shown by our measurements.</p>

2020 ◽  
Author(s):  
Francisco Cereceda-Balic ◽  
Maria Florencia Ruggeri ◽  
Victor Vidal ◽  
Humberto Gonzalez

<p>Atmospheric Black carbon (BC) strongly affects direct radiative forcing and climate, not only while suspended in the atmosphere but also after deposition onto high albedo surfaces, which are especially sensitive, because the absorption of solar radiation by deposited BC accelerate the snowpack/ice melting. In the Southern Hemisphere, the BC generated in the continents can be transported through the atmosphere from low and mid-latitudes to Antarctica, or it can be emitted in Antarctica by the anthropogenic activities developed in situ.  To assess the potential origin of the BC deposited in the snow of the Antarctic, and establish a possible relationship with the human activities that are carried out there, snow samples were taken in different sites from the Antarctic peninsula during summer periods: Chilean Base O’Higgins (BO), 2014; La Paloma Glacier 2015 and 2016 (at a distance of 6 km separated from BO); close to Chilean Base Yelcho (BY), 2018 and away from Chilean Base Yelcho 2018 (at a distance of 5 km separated from BY). Shallow snow samples were collected in Whirl-Pak (Nasco) plastics bags from the top of the snowpack, in an area of 1 m<sup>2</sup> and 5 cm thick layer, using a clean plastic shovel and disposable dust-free nitrile gloves. Sample weighed around 1500-2000 g, and they were kept always frozen (-20 °C), during transport and storage, until they could be processed in the laboratory. BC concentration in the snow samples was determined by using a novel methodology recently developed, published and patent by the authors (Cereceda et al 2019, https://doi.org/10.1016/j.scitotenv.2019.133934; US 16/690,013-Nov, 2019 ). The methodology consisted of a filter-based optical method where snow samples were microwave-assisted melted, then filtered through a special filtration system able to generate a uniform BC spot on Nuclepore 47 mm polycarbonate filters (Whatman, UK). BC deposited in filters was analyzed using a SootScan™, Model OT21 Optical Transmissometer (Magee Scientific, USA), where optical transmission was compared between the sample and a reference filter at a wavelength of 880 nm. The BC mass concentration was calculated using a 5-points calibration curve, previously prepared using real diesel BC soot as standard.  Results showed a BC concentration in snow of 1283.8 ± 1240 µg kg<sup>-1</sup>. Snow from O’Higgins Base presented the highest BC concentration (3395.7 µg kg<sup>-1</sup>), followed by snow from the site close to Yelcho Base (1309.2 µg kg<sup>-1</sup>), snow from La Paloma Glacier 2016 (745.9 µg kg<sup>-1</sup>), snow from the site away from Yelcho Base (734.5 µg kg<sup>-1</sup>) and snow from La Paloma Glacier 2015 (233.6 µg kg<sup>-1</sup>). BC values observed in Antarctic snow were higher than others previously reported in the literature (Cereceda et al 2019) and showed the influence that anthropic activities have in the study area, considering that the two highest values of BC concentration in snow were found at sites near the bases, which presented levels comparable to those found in snowy sites in the Andes, continental Chile (Cereceda et al 2019).</p>


1982 ◽  
Vol 3 ◽  
pp. 255-259 ◽  
Author(s):  
D. A. Peel ◽  
E. W. Wolff

A snow-pit and hand-drilled core have been sampled at Spaatz Island in the Antarctic Peninsula to obtain evidence on the importance of short-term fluctuations of heavy metal (Cd, Cu, Pb, and Zn) concentrations. A programme of air sampling was undertaken at the same time to investigate directly the link between concentrations in air and in snow. The snow samples and air filters have been analysed by atomic absorption spectrometry (AAS) following preconcentration on tungsten wires and by differential pulse anodic stripping voltammetry (DPASV). One sequence of snow samples was preconcentrated in the field and analysed later for Cd in the laboratory. The snow analyses confirm that year-to-year variations in heavy metal concentrations may be comparable with changes due to long-term variations in global emission rates to the atmosphere from industrial sources. The importance of understanding these apparently meteorologically controlled processes is underlined. Averaged data from the combined air/snow sampling programme show a satisfactory linear relationship between concentrations in air and in snow for both the heavy metals and for the cation component of the marine aerosol. The results, considered in the light of Junge's model for static rainout, give a ratio for concentration in air (ng m−3)/concentration in snow (ng g−1) of 0.6±0.3.


1981 ◽  
Vol 59 (1) ◽  
pp. 92-102 ◽  
Author(s):  
John L. Bengtson ◽  
Donald B. Siniff

Examination of a sample of 94 female crabeater seals collected in November, 1977, indicated that, for the past 7 years, the average age at sexual maturity was 3.8 years. Reproductive performance as evidenced by uterine scars and ovarian corpora is discussed. No females inseminated at age 4 or less successfully carried a fetus full term. Timing of ovulation was affected by both age and social category. Younger seals ovulate later in the season than older seals. No females ovulated prior to weaning their pups. Ovulation in experienced females occurred sometimes while still in a mated pair, but mostly at or after dissolution of the pair bond. Comparison of recent age of sexual maturity with earlier reports shows an increase in this age since 1967. This trend may reflect geographical differences or changes in the Antarctic marine ecosystem following a slowdown in Antarctic whaling.


Polar Science ◽  
2018 ◽  
Vol 16 ◽  
pp. 10-22 ◽  
Author(s):  
Mukunda M. Gogoi ◽  
S. Suresh Babu ◽  
Santosh K. Pandey ◽  
Vijayakumar S. Nair ◽  
Aditya Vaishya ◽  
...  

2021 ◽  
Author(s):  
◽  
Meghana Amarnath Rajanahally

<p>Sea ice algal communities play a very significant role in primary production in the Southern Ocean, being the only source of fixed carbon for all other life in this habitat and contributing up to 22% of Antarctic primary production in ice-covered regions. Therefore it is important to understand how these organisms adapt to this highly variable and harsh environment Previous studies have described their acclimation to changes in environmental conditions but we still do not understand the physiological basis of these responses. This study examines the effects of varying levels of photosynthetically active radiation (PAR), ultraviolet-B (UV-B) radiation and temperature on bottom ice algal communities and individual algal species using pulse-amplitude modulation (PAM) fluorometry, the production of mycosporine-like amino acids (MAAs) and superoxide dismutase (SOD) activity.  The experiments conducted in this thesis show that bottom ice algae are capable of acclimating to the higher levels of PAR and temperature that would likely be experienced during sea ice melt As temperature was increased past a threshold temperature of thylakoid integrity, it became the major stressor, causing decreases in photosynthetic yield at around 14°C, even at ambient PAR exposure. Similarly, a thylakoid integrity experiment independently suggested that the critical temperature for the onset of thylakoid damage was 14°C, which correlated well to the 14°C incubation observations, although this is a temperature that sea ice algae are unlikely to encounter in the polar regions.  It is likely that sea ice algae produce additional MAAs, known to be cellular sunscreens, in response to increasing levels of UV-B, allowing tolerance of this stressor. This is the first study in the marine environment to demonstrate that algae can produce MAAs in response to increasing PAR and temperature, even in the absence of UV-B, indicating that MAAs may be more than just sunscreen compounds. The levels of UV-B used in this study were representative of those likely to be faced by the algae during sea ice melt. With increasing temperature, the algae maintained photosynthetic yield and decreased MAA production, implying that the rise in temperature aids the algae with another element of photoprotection such as enzymatic repair. As these results contrasted with previous studies of bottom ice algae that showed no additional MAA production in response to higher levels of PAR and UV-B, it was hypothesized that this difference was attributed to variations in species composition that could modify the productivity of the community.  The short-term effects of increasing PAR and UV -B on three unialgal cultures of Thalassiosira sp., Fragilariopsis sp. (from the Ross Sea), and Chaetoceros sp. (from the Antarctic Peninsula) were therefore examined. In unialgal culture studies, these three algal species showed higher tolerance to PAR and UV-B compared to that of the mixed culture of bottom ice algae, although there remained species-specific variation. Both Ross Sea species showed increasing photosynthetic yield with increasing PAR and UV-B exposure, but there was a difference in the tolerance shown by the two species. Thalassiosira sp. tolerated higher PAR and lower UV-B and Fragilariopsis tolerated lower PAR and higher UV-B. Both species produced MAAs in response to these stressors, indicating that these compounds allowed the algae to decrease levels of photoinhibition.  In comparison to the Ross Sea, the Antarctic Peninsula is an area of higher environmental variability and change, meaning that the species in both regions could have varying acclimatory capabilities. Although data from three species alone cannot conclusively demonstrate that algae from different regions have different acclimatory capabilities, they do illustrate considerable variation between species. Chaetoceros sp. from the Antarctic Peninsula region showed a higher tolerance to PAR and UV-B compared to the Ross Sea species. The former species showed an increase in photosynthetic yield in response to increasing PAR and this was accompanied by a lack of MAA production in response to the experimental levels of PAR, which indicates that the two Ross Sea species have a higher tolerance to PAR compared to the Antarctic Peninsula species. Chaetoceros sp. from the Antarctic Peninsula showed an increase in photosynthetic yield in response to high UV-B exposures, accompanied by MAA production and had no signs of photoinhibition.  A further experiment was conducted to address the weaknesses in the initial methodologies, particularly related to control conditions in the short-term experiments. Common species from the Ross Sea, Antarctic Peninsula and the Arctic were exposed to a combination of increased PAR and UV-B over a period of seven days to compare acclimatory abilities using PAM and SOD activity. Thalassiosira antarctica from the Ross Sea, Chaetoceros socialis from the Antarctic Peninsula and C. socialis from the Arctic showed no significant change in quantum yield over the incubation period. This further highlights the importance of running experiments with compounding factors, as an increase in one factor could alleviate the negative effect of the other. There was an unexpected lack of change in SOD activity for all species under all treatments applied, which could indicate that the levels of PAR and UV-B used were not high enough to cause stress in these species. This work also points to the need to assay for various antioxidants, as algae are known to rely on a network of antioxidants in their defence against environmental stresses.  The data from this thesis clarify the influence of PAR, UV-B and temperature on sea ice algae, and could help better evaluate the fate of these communities under various climate change scenarios. This study has made important steps towards understanding the acclimatory abilities of sea ice algae. Increasing knowledge of sea ice algal physiology, particularly of photosynthetic health in response to environmental change, will help improve predictions of productivity in the most productive ocean on this planet. Algal tolerance to increasing PAR, UV-B and temperature is remarkable, and this ability could be crucial in the context of future climate change. The productivity of these autotrophic microorganisms strongly influences secondary production that ties their fate to that of all other life in the Southern Ocean.</p>


2021 ◽  
Author(s):  
Christian Sommer ◽  
Thorsten Seehaus ◽  
Lukas Sochor ◽  
Philipp Malz ◽  
Matthias Braun

&lt;p&gt;The large ice caps and glaciers of the northern and southern polar regions have the potential to contribute significantly to global sea-level rise, yet measurements of glacier mass changes in those regions are scarce and difficult due to harsh conditions and the size of Arctic and Antarctic glacier areas. Acquisitions of the synthetic aperture radar satellite mission TanDEM-X provide valuable insights into glacier dynamics in those regions as the X-band radar is independent from clouds and illumination and can resolve elevation changes of large glacierized areas as well as individual glaciers. We use specifically generated and coregistered digital elevation models (DEM) from repeated TanDEM-X data takes to derive glacier elevation changes between 2010 and 2020.&lt;/p&gt;&lt;p&gt;For the Arctic regions, we already calculated elevation changes for the Russian Arctic archipelagos from TanDEM-X acquisitions (2000-2017). Currently, we are preparing similar TanDEM-X DEM differences for Arctic glaciers outside the Greenland ice sheet (Svalbard, Iceland, Alaska, Canadian Arctic, Scandinavia and North Asia). In contrast to the wide and smooth areas of the East and West Antarctic ice sheets, the steep topography of the Antarctic Peninsula strongly limits the application of altimeter data for accurately quantifying glacier mass changes. Therefore, we computed glacier mass changes along the Antarctic Peninsula by means of TanDEM-X data.&lt;/p&gt;&lt;p&gt;Additionally, measurements of the IceSAT2 laser altimeter will be integrated in the analysis to improve the estimation of radar signal penetration into snow and firn and thereby reduce the elevation change and mass balance uncertainties.&lt;/p&gt;


1988 ◽  
Vol 10 ◽  
pp. 201 ◽  
Author(s):  
Alan L. Dick

Ultra-clean techniques have been used to collect a series of fresh surface-snow samples on Gipps Ice Rise, Larsen Ice Shelf (68°48′S, 60°54′W) between 21 December 1984 and 12 February 1985. Aerosol samples were collected simultaneously on to pre-cleaned membrane filters to allow the direct comparison of trace-element levels in air and snow. Samples have been analysed by various techniques for cadmium, copper, lead, zinc, aluminium, calcium, potassium and sodium. For all elements, cross-sample concentration profiles have been obtained to support the data for snow samples. The heavy-metal concentrations found in the surface snow were similar to those measured previously near Gomez Nunatak in the Antarctic Peninsula. The mean aerosol concentrations found at Gipps Ice Rise were Cd: 0.06 pg m−3, Cu: 1.0 pg m−3, Pb; 4.7 pg m−3, Zn: 6.1 pg m−3. These are the lowest concentrations measured so far in Antarctic aerosol. The ratio of the snow concentration (pg g−1) to air concentration (ng m−3), known as the washout factor, has been calculated for each element and sampling period. The data show that, for the Antarctic Peninsula, the marine aerosol is more efficiently removed to the snow-pack than is the crustal aerosol. Heavy metals are least efficiently removed. This result suggests that the measurement of concentrations in snow and ice alone may lead to misinterpretation of atmospheric source strengths.


1988 ◽  
Vol 10 ◽  
pp. 201-201 ◽  
Author(s):  
Alan L. Dick

Ultra-clean techniques have been used to collect a series of fresh surface-snow samples on Gipps Ice Rise, Larsen Ice Shelf (68°48′S, 60°54′W) between 21 December 1984 and 12 February 1985. Aerosol samples were collected simultaneously on to pre-cleaned membrane filters to allow the direct comparison of trace-element levels in air and snow. Samples have been analysed by various techniques for cadmium, copper, lead, zinc, aluminium, calcium, potassium and sodium. For all elements, cross-sample concentration profiles have been obtained to support the data for snow samples.The heavy-metal concentrations found in the surface snow were similar to those measured previously near Gomez Nunatak in the Antarctic Peninsula. The mean aerosol concentrations found at Gipps Ice Rise were Cd: 0.06 pg m−3, Cu: 1.0 pg m−3, Pb; 4.7 pg m−3, Zn: 6.1 pg m−3. These are the lowest concentrations measured so far in Antarctic aerosol.The ratio of the snow concentration (pg g−1) to air concentration (ng m−3), known as the washout factor, has been calculated for each element and sampling period. The data show that, for the Antarctic Peninsula, the marine aerosol is more efficiently removed to the snow-pack than is the crustal aerosol. Heavy metals are least efficiently removed. This result suggests that the measurement of concentrations in snow and ice alone may lead to misinterpretation of atmospheric source strengths.


2011 ◽  
Vol 5 (6) ◽  
pp. 3259-3289 ◽  
Author(s):  
A. I. Weiss ◽  
J. C. King ◽  
T. A. Lachlan-Cope ◽  
R. S. Ladkin

Abstract. This study investigates the surface albedo of the sea ice areas adjacent to the Antarctic Peninsula during the austral summer. Aircraft measurements of the surface albedo which were conducted in the sea ice areas of the Weddell and Bellingshausen Sea show significant differences between these two regions. The averaged surface albedo varied between 0.13 and 0.81. The ice cover of the Bellingshausen Sea consisted mainly of first year ice and the sea surface showed an averaged sea ice albedo of αi = 0.64 &amp;pm; 0.2 (&amp;pm; standard deviation). The mean sea ice albedo of the pack ice area in the Western Weddell Sea was αi = 0.75 &amp;pm; 0.05. In the Southern Weddell Sea, where new, young sea ice prevailed, a mean albedo value of αi = 0.38 &amp;pm; 0.08 was observed. Relatively warm open water and thin, newly formed ice had the lowest albedo values, whereas relatively cold and snow-covered pack ice had the highest albedo values. All sea ice areas consist of a mixture of a large variability of different sea ice types. An investigation of commonly used parameterizations of albedo as a function of surface temperature in the Weddell and Bellingshausen Sea ice areas showed that the albedo parameterizations don't work well in particular for areas with new, young ice. We determined typical linear temperature-albedo functions for three sea ice areas adjacent to the Antarctic Peninsula, which are reflecting the differences in the mixture of ice age, thickness and sea ice surface cover.


2020 ◽  
Vol 14 (6) ◽  
pp. 2087-2101
Author(s):  
Yukihiko Onuma ◽  
Nozomu Takeuchi ◽  
Sota Tanaka ◽  
Naoko Nagatsuka ◽  
Masashi Niwano ◽  
...  

Abstract. Surface albedo of snow and ice is substantially reduced by inorganic impurities, such as aeolian mineral dust (MD) and black carbon (BC), and also by organic impurities, such as microbes that live in the snow. In this paper, we present the temporal changes of surface albedo, snow grain size, MD, BC and snow algal cell concentration observed on a snowpack in northwest Greenland during the ablation season of 2014 and our attempt to reproduce the changes in albedo with a physically based snow albedo model. We also attempt to reproduce the effects of inorganic impurities and the red snow algae (Sanguina nivaloides) on albedo. Concentrations of MD and red snow algae in the surface snow were found to increase in early August, while snow grain size and BC were found to not significantly change throughout the ablation season. Surface albedo was found to have decreased by 0.08 from late July to early August. The albedo simulated by the model agreed with the albedo observed during the study period. However, red snow algae exerted little effect on surface albedo in early August. This is probably owing to the abundance of smaller cells (4.9×104 cells L−1) when compared with the cell abundance of red snow reported by previous studies in the Arctic region (∼108 cells L−1). The simulation of snow albedo until the end of the melting season, with a snow algae model, revealed that the reduction in albedo attributed to red snow algae could equal 0.004, out of a total reduction of 0.102 arising from the three impurities on a snowpack in northwest Greenland. Finally, we conducted scenario simulations using the snow albedo model, coupled with the snow algae model, in order to simulate the possible effects of red snow blooming on snow albedo under warm conditions in northwest Greenland. The result suggests that albedo reduction by red snow algal growth under warm conditions (surface snow temperature of +1.5 ∘C) reached 0.04, equivalent to a radiative forcing of 7.5 W m−2 during the ablation season of 2014. This coupled albedo model has the potential to dynamically simulate snow albedo, including the effect of organic and inorganic impurities, leading to proper estimates of the surface albedo of snow cover in Greenland.


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