• Journal of Geographical Sciences
  • Vol. 30, Issue 6, 969 (2020)
Yili ZHANG1,2,3,*, Xue WU1,3, and Du ZHENG1
Author Affiliations
  • 1. Key Laboratory of Environment Change and Resources Use in Beibu Gulf, the Ministry of Education, Nanning Normal University, Nanning 530001, Guangxi, China
  • 2. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China
  • 3. University of Chinese Academy of Sciences, Beijing 100049, China
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    DOI: 10.1007/s11442-020-1765-0 Cite this Article
    Yili ZHANG, Xue WU, Du ZHENG. Vertical differentiation of land cover in the central Himalayas[J]. Journal of Geographical Sciences, 2020, 30(6): 969 Copy Citation Text show less
    Maps of the study area showing the terrain (a), and the southern and northern slopes of Mt. Qomolangma determined by using three division methods: (b) ridgeline method, (c) sample transect method and (d) sector methodZ
    Fig. 1. Maps of the study area showing the terrain (a), and the southern and northern slopes of Mt. Qomolangma determined by using three division methods: (b) ridgeline method, (c) sample transect method and (d) sector methodZ
    Schematic showing the terminology used to describe the altitudinal distributions of land cover types
    Fig. 2. Schematic showing the terminology used to describe the altitudinal distributions of land cover types
    Schematic showing the vertical distributions of compound dominant land cover types (from left to right: cropland-forest dominant belt, forest-cropland dominant belt, forest dominant belt, forest-cropland dominant belt, cropland-forest dominant belt, and cropland dominant belt)
    Fig. 3. Schematic showing the vertical distributions of compound dominant land cover types (from left to right: cropland-forest dominant belt, forest-cropland dominant belt, forest dominant belt, forest-cropland dominant belt, cropland-forest dominant belt, and cropland dominant belt)
    Altitudinal distributions of different land cover types on the southern and northern slopes based on the three slope division methods: (a) sector method; (b) MM sample transect method; (c) MQ sample transect method; (d) MC sample transect method; and (e) ridgeline method
    Fig. 4. Altitudinal distributions of different land cover types on the southern and northern slopes based on the three slope division methods: (a) sector method; (b) MM sample transect method; (c) MQ sample transect method; (d) MC sample transect method; and (e) ridgeline method
    Distributions and compositions of different land cover types in different vertical zones on the northern and southern slopes based on different slope division methods: (a) southern slope, sector method; (b) northern slope, sector method; (c) southern slope, MM sample transect method; (d) northern slope, MM sample transect method; (e) southern slope, MC sample transect method; (f) northern slope, MC sample transect method; (g) southern slope, MQ sample transect method; (h) northern slope, MQ sample transect method; (i) southern slope, ridgeline method; and (j) northern slope, ridgeline method
    Fig. 5. Distributions and compositions of different land cover types in different vertical zones on the northern and southern slopes based on different slope division methods: (a) southern slope, sector method; (b) northern slope, sector method; (c) southern slope, MM sample transect method; (d) northern slope, MM sample transect method; (e) southern slope, MC sample transect method; (f) northern slope, MC sample transect method; (g) southern slope, MQ sample transect method; (h) northern slope, MQ sample transect method; (i) southern slope, ridgeline method; and (j) northern slope, ridgeline method
    Dominant altitudinal band structures of land cover types on the southern and northern slopes of the KRB based on different slope division methods: (a) sector method; (b) sample transect method with MQ, MC, and MM transects; and (c) ridgeline method. For the ridgeline method, both the southern and northern slopes contain unique distribution types in the two directions, which increase the uncertainty in the results. Therefore, the vertical zonation of land cover based on the ridgeline method is not discussed in this paper.Note: code representation in legend: 1-cropland, 2-forest, 3-shrubland, 4-grassland, 5-sparse vegetation, 6-bare land, 7-waterbody, 8-glacier/snow cover, 9-none
    Fig. 6. Dominant altitudinal band structures of land cover types on the southern and northern slopes of the KRB based on different slope division methods: (a) sector method; (b) sample transect method with MQ, MC, and MM transects; and (c) ridgeline method. For the ridgeline method, both the southern and northern slopes contain unique distribution types in the two directions, which increase the uncertainty in the results. Therefore, the vertical zonation of land cover based on the ridgeline method is not discussed in this paper.Note: code representation in legend: 1-cropland, 2-forest, 3-shrubland, 4-grassland, 5-sparse vegetation, 6-bare land, 7-waterbody, 8-glacier/snow cover, 9-none
    Land cover typeDivision methodSouthern slopeNorthern slopeArea ratio
    Area (km2)PercentageArea (km2)PercentageSouthern slope: northern slope
    CroplandSector method374.2044.945.661.0566.11︰1
    MM transect304.7527.2423.352.0813.05︰1
    MQ transect240.2919.528.210.8729.27︰1
    MC transect406.9631.889.041.0245.02︰1
    Ridgeline method*7917.9526.91243.640.9932.50︰1
    ForestSector method342.3841.12---
    MM transect516.3446.16---
    MQ transect559.9945.50---
    MC transect406.8031.87---
    Ridgeline method1117737.99262.541.0842.60︰1
    ShrublandSector method13.621.64---
    MM transect38.653.4510.410.933.71︰1
    MQ transect34.852.83---
    MC transect36.132.83---
    Ridgeline method1433.424.87660.562.692.17︰1
    GrasslandSector method22.172.66340.0862.990.07︰1
    MM transect41.973.75553.2349.380.08︰1
    MQ transect43.263.51522.0655.100.08︰1
    MC transect106.158.31450.4250.940.24︰1
    Ridgeline method2041.396.9411886.7248.400.17︰1
    Sparse vegetationSector method10.161.2269.5712.890.15︰1
    MM transect28.042.5196.748.630.29︰1
    MQ transect28.562.3272.777.680.39︰1
    MC transect66.065.1735.494.011.86︰1
    Land cover typeDivision methodSouthern slopeNorthern slopeArea ratio
    Area (km2)PercentageArea (km2)PercentageSouthern slope: northern slope
    Ridgeline method1016.773.461073.824.370.95︰1
    WaterbodySector method9.501.140.010.00950︰1
    MM transect9.670.866.900.621.40︰1
    MQ transect7.900.641.430.155.52︰1
    MC transect13.691.072.400.275.70︰1
    Ridgeline method182.870.62152.430.621.20︰1
    Construction landSector method0.320.041.170.220.27︰1
    MM transect0.190.020.480.040.40︰1
    MQ transect-----
    MC transect-----
    Ridgeline method13.680.050.790.0017.30︰1
    Bare landSector method34.374.1388.1816.330.39︰1
    MM transect87.347.81277.8824.800.31︰1
    MQ transect176.4514.34192.3220.300.92︰1
    MC transect145.7911.42203.9523.060.71︰1
    Ridgeline method4010.3313.637750.9431.560.52︰1
    WetlandSector method3.180.3814.932.770.21︰1
    MM transect8.350.7512.861.150.65︰1
    MQ transect9.070.7422.952.420.40︰1
    MC transect11.910.9381.779.250.15︰1
    Ridgeline method279.490.95787.953.210.36︰1
    Glacier/snow cover**Sector method22.832.7420.263.751.13︰1
    MM transect83.277.44138.5112.360.60︰1
    MQ transect130.4810.60127.7413.481.02︰1
    MC transect83.116.51101.1911.440.82︰1
    Ridgeline method1355.584.611740.597.090.78︰1
    TotalSector method832.73100.00539.87100.001.54︰1
    MM transect1118.57100.001120.36100.001.00︰1
    MQ transect1230.85100.00947.48100.001.30︰1
    MC transect1276.59100.00884.27100.001.44︰1
    Ridgeline method29428.43100.0024559.97100.001.20︰1
    Table 1.

    Areas and proportions of different land cover types on the northern and southern slopes

    Land cover typeDivision methodSouthern slopeNorthern slope
    Class I-Elevation range (m)Core distribution zone (m)Advantagezone (m)Elevation range (m)Core distribution zone (m)Advantagezone (m)
    CroplandSector method100-4000600-1700100-18004000-45004100-4500-
    MM transect100-40001100-22001000-17004200-46004200-4500-
    MQ transect100-4000700-1500-3900-45004300-4500-
    MC transect200-4000500-1400200-14004200-45004400-4500-
    Ridgeline method96-4300700-1700100-15002300-45004100-4500-
    ForestSector method100-4000500-20001800-3600---
    MM transect100-40001700-3100100-10001700-3900---
    MQ transect100-4000600-1900100-3700---
    MC transect200-4000700-22001400-3800---
    Ridgeline method100-40001100-26001500-38002100-40003200-40002300-3900
    ShrublandSector method1700-51003300-42003600-4000---
    MM transect1700-50003200-42003900-4100---
    MQ transect1600-50003700-42003700-42004300-53004500-5000-
    MC transect1600-51003500-43003800-4000---
    Ridgeline method300-48003400-46003800-42002400-48004200-48003900-4100
    GrasslandSector method1600-59004100-51004000-50004000-51004500-50004000-5100
    MM transect3000-51004600-51004200-51004400-49004200-5100
    MQ transect1500-51004100-50003900-51004400-50004000-5100
    MC transect2500-51004300-50004000-50004200-51004300-47004400-5000
    Ridgeline method1400-51004400-50004400-50002500-51004400-50004100-5100
    Sparse vegetationSector method3000-53004400-5300-4600-54005000-54005100-5400
    MM transect3000-53004500-5300-4700-53005000-53005100-5300
    MQ transect3300-53004100-4800-4700-53005200-53005100-5300
    MC transect3100-53004500-5200-4700-53005200-53005200-5300
    Ridgeline method2100-53004600-5300-4000-54005000-54005100-5400
    WaterbodySector method100-25004200-5300100-500-4200-45005000-58004200-4400-
    MM transect100-8001400-22004600-54004900-5400-4200-44005700-61004200-4300-
    MQ transect100-9003700-5300100-500-4200-53004200-43004800-5000-
    MC transect200-18004200-5300200-700-4200-44005500-58004300-4400-
    Ridgeline method96-29003700-5300200-7004900-5300-2200-53004100-4600-
    Construction landSector method1000-17001100-13001500-1600-4200-44004300-4400-
    MM transect------
    MQ transect1500-17001500-1600-4200-44004300-4400-
    Land cover typeDivision methodSouthern slopeNorthern slope
    Class IElevation range (m)Core distribution zone (m)Advantagezone (m)Elevation range (m)Core distribution zone (m)AdvantageZone (m)
    MC transect------
    Ridgeline method400-24001000-1600-4200-44004200-4400-
    Bare landSector method>30004800-59005000-5700> 42005100-56005400-6000
    MM transect>30005000-59004100-5500> 42005000-59005300-6100
    MQ transect>34004300-52004200-5100> 43005100-57005300-5900
    MC transect>31005000-55005000-5900> 43005000-58005000-52005300-6100
    Ridgeline method>11004700-57004200-44005000-5700>30005000-57005400-6000
    WetlandSector method< 2800100-500-4000-50004200-4500-
    MM transect< 4900100-1000-4200-52004200-4500-
    MQ transect100-4500400-1100-3900-53004000-44003900-4000
    MC transect< 5200200-1400-< 55004300-4400-
    Ridgeline method< 5100200-1400-3500-53004100-4400-
    Glacier/snow coverSector method> 44005200-5900> 5700> 51006000-6600>6000
    MM transect> 48005100-5800> 5500> 54006000-6700>6100
    MQ transect> 41005000-6000> 5100> 43005200-6300> 5900
    MC transect> 46004700-5700> 5900> 54006000-6600>6100
    Ridgeline method> 40005100-5900> 5700>38005400-6300>6000
    Table 2.

    Altitudinal distributions of different land cover types on the northern and southern slopes based on different slope division methods

    Vertical climatic zone of MQ (Zheng et al., 1975)Vertical soil zone of MQ (Gao et al., 1975)Sector method of MQDominant belt of land cover(this paper)
    Elevation (m)Vertical climatic zoneElevation (m)Vertical soil zoneAdvantage zone (m)Land cover type
    Southernslope1600-2500Mountain subtropical zone1600-2500Mountain yellow-brownsoil100-1800Cropland
    2500-3100Mountain warmtemperate zone2400-3100Mountain acid brown soil1800-3600Forest
    3100-3900Mountain cold temperate zone3100-4100Mountain bleached podolic soil3600-4000Shrubland
    3900-4700Subalpine cold zone4100-4500Subalpine shrub meadow soil
    4100-4500Subalpine meadow soil4000-5000Grassland
    4500-4800Alpine meadow soil
    4700-5500Alpine cold zone4800-5600Alpine frozen soil5000-5700Bare land
    > 5500Alpine ice-snow belt> 5600Ice and snow> 5700Glacier/snow cover
    Northern slope4000-5000Plateau cold zone4400-4700Subalpine steppe soil4000-5100Grassland
    5000-6000Alpine cold zone4700-5200Alpine meadow-steppe soil5100-5400Sparse vegetation
    5200-5500Alpine frozen soil5400-6000Bare land
    > 6000Alpine ice-snow belt> 5500Ice and snow> 6000Glacier/snow cover
    Table 3.

    Comparison of the altitudinal distributions of land cover, climate, and soil on the southern and northern slopes of Mt. Qomolangma

    Vertical distributions of land cover types (this paper)Vertical distributions of vegetation(Zhang et al., 1973)
    Advantage zone (m)Land cover typesDistribution range (m)Vegetation types
    100-1800Cropland< 1000 (1200)Monsoon forest zone
    Southern slope1000-25002500-3000 (3100)Evergreen broadleaved forest beltMountain coniferous broadleaved (evergreen,deciduous) mixed-forest zone
    1800-3600Forest
    3000-3800 (4100)Subalpine coniferous zone
    3600-4000Shrubland3800-(4100)-4500Alpine brush
    4000-5000Grassland4500-5200Alpine meadow.
    Sparse vegetation
    5000-5700Bare land5200-5500 (5600)Lichen gravel zone
    > 5700Glacier/snow cover> 5500 (5600)Permanent snow-ice zone
    4000-5100Grassland3900-4400Steppe zone
    Northern slopeGrassland4400-5000Alpine steppe zone
    5100-5400Sparse vegetation5000-5700Alpine meadows with sparse cushion vegetation zones
    5400-6000Bare land
    5700-5800-(6200)Lichen, gravel zone
    > 6000Glacier/Snow cover> 5800-6200Frigid zone
    Table 4.

    Comparison of the vertical distributions between land cover types and vegetation on the slopes of Mt. Qomolangma

    Yili ZHANG, Xue WU, Du ZHENG. Vertical differentiation of land cover in the central Himalayas[J]. Journal of Geographical Sciences, 2020, 30(6): 969
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