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Original Articles

n-Alkanes in Fresh Snow in Hokkaido, Japan: Implications for Ice Core Studies

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Pages 119-131 | Accepted 01 Sep 2012, Published online: 05 Jan 2018

Figures & data

FIGURE 1. Snow sampling sites in Hokkaido, Japan.

FIGURE 1. Snow sampling sites in Hokkaido, Japan.

FIGURE 2. n-Alkane distributions in the snow samples and the corresponding 5-day back trajectories for each sampled snowfall event in Sapporo. Sampling dates for S1–S8 are given in .

FIGURE 2. n-Alkane distributions in the snow samples and the corresponding 5-day back trajectories for each sampled snowfall event in Sapporo. Sampling dates for S1–S8 are given in Table 1.

FIGURE 3. n-Alkane distributions in the snow samples and the corresponding 5-day back trajectories for each sampled snowfall event in Moshiri. Sampling dates for M1–M9 are given in .

FIGURE 3. n-Alkane distributions in the snow samples and the corresponding 5-day back trajectories for each sampled snowfall event in Moshiri. Sampling dates for M1–M9 are given in Table 1.

TABLE 1 Sample information and n-alkane ranges, concentrations, and distributions in the Sapporo and Moshiri samples. ACL = average chain length, CPI = carbon preference index.

FIGURE 4. Total concentrations of the n-alkanes in the Sapporo snow samples (S1–S8), given as ng/L (meltwater).

FIGURE 4. Total concentrations of the n-alkanes in the Sapporo snow samples (S1–S8), given as ng/L (meltwater).

FIGURE 5. Total concentrations of the n-alkanes in the Moshiri snow samples (M1–M9), given as ng/L (meltwater).

FIGURE 5. Total concentrations of the n-alkanes in the Moshiri snow samples (M1–M9), given as ng/L (meltwater).

FIGURE 6. (a) Urban area extent in Asia, as the percentage of urban 0.5 × 0.5 km pixels in 5 × 5 km bins, (b) Land use classes and urban areas in Asia. Data for both parts a and b are from the MODIS 500-m global map of urban extent (CitationSchneider et al., 2009, Citation2010). In part b, several land use classes are combined: forest includes all forest types (1–5); shruband grasslands include open and closed shrublands, savannas, and grasslands (6–10); and a land use class defined as a mosaic of crops and other land cover types is included in croplands (12,14). Numbers refer to the International Geosphere-Biosphere Programme (IGBP) scheme of 17 land use classes, (c) Distribution of C4 vegetation in Asia (CitationStill et al., 2009).

FIGURE 6. (a) Urban area extent in Asia, as the percentage of urban 0.5 × 0.5 km pixels in 5 × 5 km bins, (b) Land use classes and urban areas in Asia. Data for both parts a and b are from the MODIS 500-m global map of urban extent (CitationSchneider et al., 2009, Citation2010). In part b, several land use classes are combined: forest includes all forest types (1–5); shruband grasslands include open and closed shrublands, savannas, and grasslands (6–10); and a land use class defined as a mosaic of crops and other land cover types is included in croplands (12,14). Numbers refer to the International Geosphere-Biosphere Programme (IGBP) scheme of 17 land use classes, (c) Distribution of C4 vegetation in Asia (CitationStill et al., 2009).

FIGURE 7. Average chain length (ACL, a unitless number) and wax percentage (%) in the Moshiri snow samples (M1–M9).

FIGURE 7. Average chain length (ACL, a unitless number) and wax percentage (%) in the Moshiri snow samples (M1–M9).

TABLE 2 Stable carbon and hydrogen isotopic composition of the n-alkanes in the Sapporo and Moshiri samples. V-SMOW = Vienna Standard Mean Ocean Water, and V-PDB = Vienna Pee Dee Belemnite.

FIGURE 8. δ13C and δD for C27 in the Sapporo snow samples (S1–S8). V-SMOW = Vienna Standard Mean Ocean Water, and V-PDB = Vienna Pee Dee Belemnite.

FIGURE 8. δ13C and δD for C27 in the Sapporo snow samples (S1–S8). V-SMOW = Vienna Standard Mean Ocean Water, and V-PDB = Vienna Pee Dee Belemnite.

FIGURE 9. δ13C and δD for C27 in the Moshiri snow samples (M1–M9). V-SMOW = Vienna Standard Mean Ocean Water, and V-PDB = Vienna Pee Dee Belemnite.

FIGURE 9. δ13C and δD for C27 in the Moshiri snow samples (M1–M9). V-SMOW = Vienna Standard Mean Ocean Water, and V-PDB = Vienna Pee Dee Belemnite.

FIGURE 10. δD for C27 in individual vegetation samples as a function of latitude. Measurements from existing literature (CitationBi et al., 2005; CitationChikaraishi and Naraoka, 2003; CitationSachse et al., 2006; CitationSmith and Freeman, 2006) as well as previously unpublished measurements by Sankelo and Seki are shown. The area shaded gray represents the range of δD values for C27 in the Hokkaido (Sapporo + Moshiri) snow samples.

FIGURE 10. δD for C27 in individual vegetation samples as a function of latitude. Measurements from existing literature (CitationBi et al., 2005; CitationChikaraishi and Naraoka, 2003; CitationSachse et al., 2006; CitationSmith and Freeman, 2006) as well as previously unpublished measurements by Sankelo and Seki are shown. The area shaded gray represents the range of δD values for C27 in the Hokkaido (Sapporo + Moshiri) snow samples.

FIGURE 11. δD for C27 in surface soil samples (CitationRao et al., 2009; circles) and in the Hokkaido (Sapporo+ Moshiri) snow samples (diamonds) as a function of latitude.

FIGURE 11. δD for C27 in surface soil samples (CitationRao et al., 2009; circles) and in the Hokkaido (Sapporo+ Moshiri) snow samples (diamonds) as a function of latitude.

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