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Research Article

Dissolved organic carbon in Alaskan Arctic snow: concentrations, light-absorption properties, and bioavailability

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Pages 1-19 | Received 15 Nov 2018, Accepted 02 Jun 2020, Published online: 26 Jun 2020

Figures & data

Fig. 1. Distribution of (a) DOC (mg L−1), (b) TN (mg L−1), (c) BC (μg L−1), and (d) major ions (μg L−1) in Alaskan snow cover in the spring of 2017. (Detailed sampling information can be referred to supplementary Table S1.).

Fig. 1. Distribution of (a) DOC (mg L−1), (b) TN (mg L−1), (c) BC (μg L−1), and (d) major ions (μg L−1) in Alaskan snow cover in the spring of 2017. (Detailed sampling information can be referred to supplementary Table S1.).

Table 1. DOC concentrations measured in snow of Alaska and Barrow and comparison with previous studies.

Fig. 2. Vertical variations of DOC concentrations and other parameters recorded in the snowpack at Barrow, Alaska.

Fig. 2. Vertical variations of DOC concentrations and other parameters recorded in the snowpack at Barrow, Alaska.

Fig. 3. Comparison of DOC (mg L−1), TN (mg L−1), BC (μg L−1), and major ions (μg L−1) in surface and subsurface snow cover at Barrow.

Fig. 3. Comparison of DOC (mg L−1), TN (mg L−1), BC (μg L−1), and major ions (μg L−1) in surface and subsurface snow cover at Barrow.

Table 2. Absorption Ångström Exponent (AAE330 − 400) and mass absorption cross section of DOC in snow across Alaska and at Barrow, as well as a comparison with other studies on snow and aerosols from other regions.

Fig. 4. Relationship between (a) MACDOC365 values and DOC concentrations, (b) MACDOC365 values and AAE330-400, and (c) SUVA254 and DOC concentrations for Alaskan snow samples, and temporal variation in MACDOC365 values (d), and SUVA254 Values (e) in snow cover on the sea ice at Barrow during the study period of April to May in 2017.

Fig. 4. Relationship between (a) MACDOC365 values and DOC concentrations, (b) MACDOC365 values and AAE330-400, and (c) SUVA254 and DOC concentrations for Alaskan snow samples, and temporal variation in MACDOC365 values (d), and SUVA254 Values (e) in snow cover on the sea ice at Barrow during the study period of April to May in 2017.

Fig. 5. Variation for ratios (a) of RF by DOC to BC, and relationships between ratios of RF by DOC to BC and (b) MACDOC365 and (c) ratios of DOC/BC in the snow at Barrow, Alaska.

Fig. 5. Variation for ratios (a) of RF by DOC to BC, and relationships between ratios of RF by DOC to BC and (b) MACDOC365 and (c) ratios of DOC/BC in the snow at Barrow, Alaska.

Fig. 6. Exponential decrease of DOC concentrations in snow cover on Chukchi sea ice during the biodegradation experiment in May of 2017 at Barrow.

Fig. 6. Exponential decrease of DOC concentrations in snow cover on Chukchi sea ice during the biodegradation experiment in May of 2017 at Barrow.

Fig. 7. Footprint analyses of the backward trajectories launched over the snow sampling site at Barrow, Alaska, during April and May in 2017 for pass by (a) 48 h and (b) 120 h, respectively, and HYSPLIT model seven day back trajectories for air masses arriving in Barrow on (c) April 17, 2017 and (d) May 2, 2017. (Different colors of backward trajectories in c and d represent the air mass arrived at the different date.).

Fig. 7. Footprint analyses of the backward trajectories launched over the snow sampling site at Barrow, Alaska, during April and May in 2017 for pass by (a) 48 h and (b) 120 h, respectively, and HYSPLIT model seven day back trajectories for air masses arriving in Barrow on (c) April 17, 2017 and (d) May 2, 2017. (Different colors of backward trajectories in c and d represent the air mass arrived at the different date.).

Table 3. Principal component analysis of DOC with other parameters in snow over across the Alaska and on sea ice at Barrow.

Fig. 8. Biplot analyses of DOC with other parameters for (a) snow samples in Barrow, and (b) snow samples across Alaska.

Fig. 8. Biplot analyses of DOC with other parameters for (a) snow samples in Barrow, and (b) snow samples across Alaska.