25 October 2019, Volume 41 Issue 5
    

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  • ZHANG Shasha, ZHANG Zhen, LIU Shiyin, LI Xin, HUANG Danni, XUE Naiting
    Journal of Glaciology and Geocryology. 2019, 41(5): 1015-1025. https://doi.org/10.7522/j.issn.1000-0240.2019.1150
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    In order to explore the terrain and altitude parameters affecting the seasonal and annual average flow velocity of glaciers, we extracted respectively the flow velocity of glaciers and the terrain factor from 2013-2018 GoLive and ASTER GDEM V2 data, integrated the regional terrain (slope gradient, aspect, altitude) and flow velocity of 3 389 glaciers in northwest of the Karakoram Mountains. It is found that the surface velocity of glacier reaches the fastest at the equilibrium line altitude (3 970-4 770 m), which is a manifestation of the glacier's positive mass balance. In the gentle area, the variation range is obviously dependent on altitude. However, the speed of glacier flow in different slope gradient areas has the same trend depending on altitude, first increasing and then decreasing. In this area, the glacier flow velocity on the north was relatively stable, while on the south (0.25 m·d-1) and the southwest (0.25 m·d-1), it was the fastest with a large amplitude of variation and a difference about 4 times between the minimum value and the maximum value. The glacier flow velocity does not show a single seasonal change, but also a dependence on terrain. The glacier flow velocity in the low altitude area is relatively fast during ablation (March to June), but in the middle altitude area, the glacier flow velocity is relatively fast before ablation (November to February).
  • LI Linfeng, LI Kaiming
    Journal of Glaciology and Geocryology. 2019, 41(5): 1026-1035. https://doi.org/10.7522/j.issn.1000-0240.2019.0533
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    Taking the Shiyang River basin of Gansu Province as the research area, using GIS and RS technologies combined with manual visual interpretation, the glacier boundary remote sensing images were extracted of 1995, 2002, 2009, 2015 and 2016. Three terrain factors, i.e., slope, orientation and elevation, are extracted, in combine with DEM data. Based on correlation analysis and GeoDetector, the correlation between glacier change and topographic factor was analyzed, and the spatial relationship between glacier change and topographic factors was studied. The results show that:(1) the annual average area change rate of glaciers in the region had changed from -1.27%·a-1 in 1973-1995 to -2.87%·a-1 in 2015-2016; the ablation rate had accelerated, and the small glaciers with an area less than 0.1 km2 had retreated significantly; (2) the main orientations of glacial distribution in the Basin were N, NE and NW, which had a certain correlation with the change of the glaciers; but those on the south slopes had retreated faster; (3) the slope had related to the change of glacier, so did the altitude, which had controlled the ablation rate of glaciers; the lower the altitude, the fast the glacier retreating; (4) the influence of topographic factors on spatial differentiation of glacial changes was significantly different; altitude was the most control factor for spatial differentiation of glacial changes, followed by orientation and then by slope.
  • LI Lin, Bianba Ciren, ZHAO Wei, Luosang Langjie, DA Ping, Zhaxi Ouzhu
    Journal of Glaciology and Geocryology. 2019, 41(5): 1036-1043. https://doi.org/10.7522/j.issn.1000-0240.2019.0532
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    The Nyang Qu Basin is a relatively developed area of agriculture in the Tibet Autono-Mous Region, and it is also a region with more glaciers. On one hand, the glacial Melt water is an important source for surface runoff, on other hand, the flood disasters caused by the glacial lake outburst threaten the lower reaches of the Nyang Qu. One of the examples is the outburst of the Sangwang Co on July 16, 1954 which caused a great damage and casualties. In this study, based on the images of the Landsat TM/ETM+ (1987-2018), the QUICKBRID (2015) and the Gofen-1 satellite (2018) as well as the topographic geological data measured in the field, we analyze the changes and the outburst characteristics of two glacial lakes, Sanwang Co and Shimo Co. The results show:during the period from 1987 to 2018, both Sangwang Co and Shimo Co were expanded, with an increase of 0.31 km2(5.56%) and 0.954 km2(96.9%) respectively. The rate of change is 0.054 km2·(10a)-1 and 0.311 km2·(10a)-1. The lateral moraine and terminal moraine of the two Lakes are uncompact sediment with loose structure and poor stability. The outlet of Sangwang Co is wide and the water is flowing smoothly. There is no direct water outflow from Shimo Co, but seepage from the innermost side of terminal moraine. The Sangwang Co and Shimo Co are connected with the ice glaciers of the trailing edge glacier. The ice tongues are steep that may have high possibility of ice collapse. Meanwhile, risks of outburst exist for both lakes due to the poor stability of the lateral moraines. The risk of outburst for Shimo Co is higher than that for Sangwang Co.
  • LI Zongxing, FENG Qi, LI Zongjie, Lü Yuemin, YUAN Ruifeng, GUI Juan, LI Yongge, ZHANG Baijuan, XUE Jian
    Journal of Glaciology and Geocryology. 2019, 41(5): 1044-1052. https://doi.org/10.7522/j.issn.1000-0240.2019.1154
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    This study has analyzed preliminary progress in the study of stable isotope ecohydrology based on systematic observation and continuous sampling in the northern slopes of the Qilian Mountains since 2012. The results showed that:sub-cloud evaporation and water vapor recycling are important for the evolution mechanisms of stable isotope of precipitation in the study area. When precipitation is higher, sub-cloud evaporation of falling raindrops will be lower and enrichment of δ18O is weaker. Therefore, rainfall events with higher precipitation amounts had more depleted δ18O and vice versa. The stable isotope of river and groundwater is stable within the year, contrast with the significant annual fluctuation in precipitation stable isotopes, which reflects the transformation from snow melt water to groundwater in glacier terminus, from supra-permafrost water to surface water in permafrost regions, and repeated transformation of surface water and groundwater in vegetation zone. Under the background of climate warming, with the intensification of evapotranspiration in alpine regions, water vapor recycling is gradually accelerating, which becomes the main transformation from gaseous water to liquid water. Meanwhile, it is an important component of water vapor source for regional precipitation. Water vapor recycling contributes about 24% of precipitation in mountainous regions above 2 000 m a.s.l. About 4/5 of the runoff is recharged in the cryosphere belt above 3 600 m a.s.l. in the northern slopes of the Qilian Mountains. The contribution of atmospheric precipitation, supra-permafrost water and glacier and snow meltwater to runoff in the outlet is 70%, 22% and 8%, respectively. The Qilian Mountains National Park is located in 95°-103.5°E, 36.8°-39.6°N, with a total area of 4.8×104 km2 (accounting for 27% of the total area of the Qilian Mountains). This result has clarified the hydrological process indicated by stable isotopes in the inland river basins under the background of climate warming and intense cryosphere ablation, provided a new basis to measure the strengthening of water vapor recycling in alpine regions, quantified the contribution ratio of water vapor recycling precipitation, and proved the fact that the contribution ratio of cryospheric meltwater to runoff variations. In particular, it has provided scientific support and technical guidance for establishing the Qilian Mountains National Park.
  • DAI Sheng, BAO Guangyu, QI Guiming, MA Zhanliang, BAI Wenrong, YU Di, FENG Xiaoli, YANG Yanhua, SHI Shengbo
    Journal of Glaciology and Geocryology. 2019, 41(5): 1053-1066. https://doi.org/10.7522/j.issn.1000-0240.2019.0901
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    Based on the extreme climatic factors in the Qilian Mountains of Qinghai Province and the hydrological data of the Qinghai Lake, the Hara Lake and some main rivers, the study shows that strong wind (gale) days had decreased significantly. The annual precipitation in Qinghai Qilian Mountains had increased most significantly in the early 21st century and changed abruptly, the increase range of precipitation in the middle and west sections had been larger than that in the east section. Annual precipitation days of daily precipitation more than 5 mm, 10 mm and 25 mm had increased significantly, especially at the beginning of the 21st century. However, days of precipitation more than 0.1 mm had decreased. The annual average strong wind days had been negatively correlated with the lake water-level fluctuation and river runoff. Reduction of strong wind days had alleviated water loss due to evaporation on lake surface and ground surface, improving vegetation had increased runoff generation and increased runoff into lakes. Precipitation had been positively correlated with lake water-level fluctuation and river runoff. Influenced by the increase of precipitation in the 21st century, the water level of the Qinghai Lake rises year by year, which has totally risen 1.67 m, reaching the water level in the late 1970s. In recent years, the runoff of the main rivers in the middle and west sections has also reached the maximum, while the runoff increase in the east section is not obvious. The annual average cumulative precipitations of more than 5 mm, 10 mm and 25 mm in the Qinghai Qilian Mountains is positively correlated with the flow of lakes and rivers, and the cumulative precipitations contribute significantly to the increase of lake water-level fluctuation and river runoff.
  • YANG Guiqian, XIE Changwei, WANG Wu, DU Erji, LIU Wenhui, ZHANG Yuxin, NI Jie
    Journal of Glaciology and Geocryology. 2019, 41(5): 1067-1077. https://doi.org/10.7522/j.issn.1000-0240.2019.0328
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    Transient electromagnetic method (TEM) has achieved a good result in permafrost investigation in the Tibetan Plateau and Northeast China, but it is limited to the case of thick sediment layers. It is basically blank to sound permafrost under the condition of shallow bedrock. Maxian Mountain permafrost in Lanzhou has the characteristics of small distribution range, high temperature and shallow bedrock. It is an ideal area for sounding permafrost distribution under shallow bedrock by TEM. In this paper, Maxian Mountain permafrost is taken as the main research object, seasonally frozen ground is taken as the contrast to study the characteristics of transient electromagnetic response. Combined with regional structural characteristics, stratum outcrop, borehole core and geothermal monitoring data, the effect of TEM sounding permafrost in shallow bedrock is demonstrated and discussed. The results show that the distribution of permafrost in the Maxian Mountain is controlled by the low resistance zone formed by tectonic faults, and the lower part is the negative temperature rock 0.11 km2. When TEM is applied to the exploration of permafrost in shallow bedrock, it responds more to the underground rock layer, which can be combined with the information of geology, geomorphology, hydrology and vegetation. The distribution of permafrost can be judged by the characteristics of soil and the variation of resistivity. When the bedrock is very shallow, it can be inverted jointly with ground penetrating radar data, borehole and other means to identify permafrost and underlying bedrock accurately.
  • WEI Yanjing, WEN Zhi, GAO Qiang, ZHANG Mingli, SHI Rui, KONG Sen
    Journal of Glaciology and Geocryology. 2019, 41(5): 1078-1086. https://doi.org/10.7522/j.issn.1000-0240.2019.0326
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    In the paper, with different pipeline temperatures set, a thermal model of the interaction between pipeline and permafrost is established to investigate the influence of chilled pipelines on the freezing and thawing of soil around pipeline and thermal stability of permafrost. The results show that warm gas pipeline of 5℃ could decrease the value of permafrost table below pipeline about 11 times diameter and aggravate the degradation of permafrost around pipeline; gas pipeline of 0℃ will expand the range of high-temperature unstable permafrost below the pipeline, decreasing the strength and bearing capacity of frozen soil below the pipeline, which is not conducive to maintaining permafrost and pipeline operation stability; -1℃ and -5℃ chilled gas pipeline can effectively improve the permafrost table and maintain the temperature stability of frozen soil below pipeline, but the temperature of soils below pipeline of -5℃ decreases obviously, which may lead to frost heave of soil. In terms of thermal stability around pipeline, the chilled gas transmission technology can protect permafrost and can be applied to the gas pipeline construction in permafrost region of Qinghai-Tibet Plateau.
  • WANG Qingzhi, FANG Jianhong, CHAO Gang, XUE Zhaofeng
    Journal of Glaciology and Geocryology. 2019, 41(5): 1087-1097. https://doi.org/10.7522/j.issn.1000-0240.2019.0325
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    In order to study the thermal stability of subgrade with different pavement types in warm-temperature permafrost region, this paper analyses the changes of temperature, heat flux, heat budget, freeze-thaw cycles and permafrost table variation of block-stone subgrade with asphalt concrete pavement and cement concrete pavement, based on the temperature data. It is found that both asphalt concrete pavement and cement concrete pavement have great influence on the temperature of block-stone subgrade, but the influence degree and depth of asphalt concrete pavement are much greater than that of cement concrete pavement. The central heat budget of block-stone subgrade on the rising trend, while the rising rate with cement concrete pavement is greater than that with asphalt concrete pavement. And the heat budget on the sunny slope of subgrade is larger than that on the shady slope. Whether the pavement material is asphalt concrete pavement or cement concrete pavement, there is no obvious melting interlayer between the left and right shoulders of subgrade. However, the permafrost is still deteriorating, and the permafrost table of the sunny slope is obviously faster than that on the shady slope. Compared with ordinary roadbed, the existence of block-stone layer can greatly raise or slow down the declining of permafrost table, and light-colored cement concrete pavement is more conducive to the thermal stability of subgrade.
  • REN Jingquan, LIU Yuxi, WANG Dongni, MU Jia, LI Xingyang, CUI Jialong, GUO Chunming
    Journal of Glaciology and Geocryology. 2019, 41(5): 1098-1106. https://doi.org/10.7522/j.issn.1000-0240.2019.1153
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    In order to understand the response frost depth of seasonally frozen soil to climate change, based on the meteorological data about daily air temperature, surface temperature, snow cover depth and frost depth from 46 meteorological stations in Jilin Province from 1961 to 2015, the spatial-temporal distribution of frost depth of seasonally frozen soil in Jilin Province and its response to air temperature and snow cover were studied through the method of linear tendency estimation and abrupt change analysis. The result showed that the maximum frost depth decreased gradually from west to east, the maximum frost depth of most stations showed a downward trend. Frozen soil occurred mainly from October to June, and the annual maximum frost depth almost always occurred in March. The frost depth varied greatly in the west, followed by the middle and the east. From 1961 to 2015, the maximum frost depth had decreased significantly at a rate of -5.8 cm·(10a)-1. The maximum frost depth had basically decreased years by years. Since the 1990s, the maximum frost depth has decreased significantly. The maximum frost depth changed abruptly in 1987, and then decreased by 22.2 cm. The frost depth was sensitive to air temperature, and the maximum frost depth of most stations was negatively correlated with average air temperature. In terms of annual variation, the rise of temperature was the main reason for the decrease of maximum frost depth. During the stable frost period of seasonally frozen soil, the ground surface was covered with snow; when the snow depth exceeded 10 cm, the effect of heat preservation become stronger gradually; when the snow depth reached 20 cm, the effect of heat preservation was more significant and the frost depth was lesser.
  • HE Binbin, SHENG Yu, HUANG Long, HUANG Xubin, ZHANG Xiyan
    Journal of Glaciology and Geocryology. 2019, 41(5): 1107-1114. https://doi.org/10.7522/j.issn.1000-0240.2019.0322
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    Annual mean freezing index and thawing index for 49 stations in north Xinjiang were calculated based on daily mean temperature from 1961 to 2017, and their variation trends and distribution characteristics were analyzed. The results showed that freezing index in North Xinjiang showed an obvious decreasing trend at a rate of 51.6℃·d·(10a)-1, ranging from 509 to 2 304.9℃·d, with an average value of 1 240℃·d. Thawing index showed an increasing trend with a rate of 73.9℃·d·(10a)-1, ranging from 526.4 to 4 531.1℃·d, with an average of 3 516℃·d. Freezing index was smaller in Junggar Basin and Yining Prefecture characterized by lower latitude and elevation, and larger in high elevation areas, such as Altai and Tianshan Mountains, while thawing index was opposite. Freezing index was dependent on longitude, latitude and elevation, while thawing index was mainly controlled by elevation in north Xinjiang. It was also found that there was a distinct linear relationship between annual mean temperature and freezing and thawing index.
  • CUI Honghuan, QIN Xiaopeng, WANG Wentao, WANG Panpan
    Journal of Glaciology and Geocryology. 2019, 41(5): 1115-1121. https://doi.org/10.7522/j.issn.1000-0240.2019.0321
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    In order to explore the influence of strength and microscopic characteristics of unsaturated silty clay in freezing-thawing conditions, freezing-thawing cycle test, unsaturated soil direct shear test and nitrogen adsorption test were carried out on the unsaturated silty clay in subgrade. The results showed that the strength of unsaturated soil decreases first and then tends to be stable with the increase of freezing-thawing cycle; when the temperature is -10℃, the cohesive force decreases most obviously; the specific surface area of the sample obtained by BET method is controlled by external conditions. According to the nitrogen isothermal adsorption test, the fractal dimension of unsaturated subgrade soil is calculated. The specific surface area and fractal dimension of the test sample first increase, then decrease with the increase of freeze-thaw cycles. The fractal dimension reaches its maximum when freeze-thaw cycles are 3 and decreases with temperature decrease. The influence of matric suction on the cohesion of unsaturated subgrade silty clay after several freezing-thawing cycles is explained from microscopic perspective.
  • XUE Ke, WEN Zhi, MA Xiaohan, ZHANG Mingli, GAO Qiang, SUN Nan
    Journal of Glaciology and Geocryology. 2019, 41(5): 1122-1129. https://doi.org/10.7522/j.issn.1000-0240.2019.0327
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    The microscopic pore characteristics of frozen soil are the basic parameters for determining a series of physical and mechanical properties of frozen soil. The volume of ice crystals in frozen soil changes with temperature, which will affect the microstructures and pore characteristics of frozen soil. Using the newly scanning electron microscope (SEM), which can be used for the research of frozen soil, to analyze the microstructure changes of Qinghai-Tibet red clay and Lanzhou silt before and after freezing under different initial conditions. It was found that ice crystal growth squeezing the surrounding soil particles when freezing. As a result, the surrounding soil particles moved and the original soil structure was damaged, the number of large pores in the soil had increased. In addition, the surrounding small pore replenished water to the ice crystals in the larger pore and made it continue to grow, due to the volume of some individual large pores increasing. After freezing, the porosity decreased and the average diameter of pores increased. In addition, for the soils with different gradations, the effect of freezing on pore size, shape and arrangement in fine-grained soils was greater than that on coarse-grained soils. Similarly, the higher the initial water content was, the greater effect of freezing on soil microstructure was. The initial water content determined the amount of ice crystals which participate in changing soil microstructures during freezing. This results reveal the effect of freezing on soil microstructures under different initial conditions, provide theoretical basis and experimental support for the study of the macro-mechanical properties and frost heave mechanism.
  • JIA Hailiang, DING Shun, WANG Ting, LUO Tao, YANG Gengshe
    Journal of Glaciology and Geocryology. 2019, 41(5): 1130-1137. https://doi.org/10.7522/j.issn.1000-0240.2019.0323
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    Frost damage of natural rock is usually controlled by moisture content rather than thermal conditions. However, more attention was paid to the thermal conditions in existing studies, the moisture condition of rocks in natural environments were rarely studied. In this paper, an indoor experiment was designed to simulate the process of surface snowmelt infiltrating into bedrock. The moisture distribution profiles before and after snowmelt infiltration were precisely measured through the layered moisture content tests via nuclear magnetic resonance method (NMR). The results indicate that:(1) The melting rate of snow and infiltrating rate of snowmelt are primarily determined by the pore structure of rock; the open macroscopic fissures is the ideal channel for snowmelt infiltration; larger porosity corresponds to faster snowmelt infiltration; in the case of similar porosities, pore connectivity controls the rate of snowmelt infiltration. (2) Water distribution across the sample is not uniform, water saturation degree at different layers of the sample differs significantly. (3) The overall saturation degrees of some samples when snowmelt infiltration do not reach to the threshold value for frost damage. Considering that the conditions of snowmelt infiltration in natural environments are more rigorous, moisture condition of rock can become a key factor in controlling the occurrence and evolution of frost damage.
  • HUANG Xiaodong, LI Xubing, LIU Changyu, ZHOU Minqiang, WANG Jianshun
    Journal of Glaciology and Geocryology. 2019, 41(5): 1138-1149. https://doi.org/10.7522/j.issn.1000-0240.2019.0529
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    Snow cover is an important parameter of surface characteristics, which has an important impact on radiation budget, climate and long-term weather changes. Snow itself is an important weather phenomenon, and is an important hydrometeorological parameter, but also brings disastrous weather and hydrological disasters, such as pastoral snow disaster, avalanches and snowmelt floods. Therefore, the monitoring of snow, especially the monitoring of snow in mountain areas, is of great significance in many aspects. The use of satellite remote sensing technology to monitor snow cover has a history of more than 30 years, and has formed operational products. With the development of remote sensing technology, the corresponding monitoring methods are also in the process of continuous development and progress. The snow cover in Qinghai-Tibet Plateau is of great hydrological, climatic and ecological significance. Therefore, the research on snow parameters extraction of the specific area on the Qinghai-Tibet Plateau by using remote sensing technology, not only can effectively improve snow monitoring accuracy, in order to evaluate the snow cover change accurately, but also can provide more accurate input snow factors for hydrology and climate models, and enhance the contribution of snow research of China in the world. The Qinghai-Tibet Plateau has an average altitude above 4 000 m. The ground observation stations are rare in this plateau. Affected by strong solar radiation and complex terrain, the rapid melting of snow, regional difference ablation and wind blowing snow and other factors lead to the serious fragmentation of snow cover distribution, which makes it difficult and uncertain to use remote sensing data to monitor the snow cover in this area. With the progress of satellite and sensor technologies, especially a series of FY satellite launch and run successfully in China, the synchronization observe technology by optical and passive microwave remote sensing is already mature. Effectively use the advantage of higher spatial resolution of optical remote sensing data and cloud penetration of passive microwave remote sensing data, combined with machine learning, UAV and other technologies, will be an effective way to improve the accuracy of snow parameters inversion in Qinghai-Tibet Plateau.
  • SHEN Liucheng, WU Tao, YOU Qinglong, JIANG Guojun, XIE Xuefeng, ZHU Lidong, YIN Jingwen
    Journal of Glaciology and Geocryology. 2019, 41(5): 1150-1161. https://doi.org/10.7522/j.issn.1000-0240.2019.1100
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    Based on daily snow depth, monthly precipitation and air temperature data, spatial and temporal characteristics of snow depth and their causes are analyzed using mathematical statistics over the central and eastern Tibetan Plateau from 1961 to 2014. The results show that spatial distribution of snow depth in the plateau is uneven. And three high-value areas of snow depth appear over the plateau, i.e. the south slopes of the Himalayas in the southwestern Tibetan Plateau, Nyainqen Tanggula-Tanggula-Bayan Har-Anyemaqen in the central Tibetan Plateau and the Qilian Mountains in the northeastern Tibetan Plateau. Snow depth reaches the maximum in winter, followed by spring and autumn, and snow depth records only take place at high altitude or latitude in summer. Snow depth is mainly reducing in the long run, especially in summer and autumn. In the background of warming and wetting over the Tibetan Plateau, the snow depth firstly increases and then decreases, but not continuously. Snow depth increases with altitude, but the maximum snow depth does not appear at the highest altitude. Snow depth in winter is dominated by precipitation, but in the other seasons is dominated by air temperature. The increase of snow depth in winter and spring during 1961-1998 had related to the increase of precipitation. But both of increasing air temperature and decreasing precipitation have caused the decrease of snow depth after 1998. The continuous reduction of snow depth in summer and autumn is related to the continuous increase of air temperature during the same period.
  • GAO Yang, HAO Xiaohua, HE Dongcai, HUANG Guanghui, WANG Jian, ZHAO Hongyu, WEI Yarui, SHAO Donghang, WANG Weiguo
    Journal of Glaciology and Geocryology. 2019, 41(5): 1162-1172. https://doi.org/10.7522/j.issn.1000-0240.2019.1155
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    The sixth version of MODIS (V6), released by the National Snow and Ice Data Center (NSIDC), offers only normalized difference snow index (NDSI). Users are often concerned about snow cover or fraction of snow cover. NSIDC recommends the world's best snow cover NDSI threshold of 0.4, but the terrain of the Tibetan Plateau is complex, the characteristics of snow patching are obvious, and a single NDSI threshold does not accurately identify snow on different land cover types. Different types of land cover may affect the NDSI threshold. Based on the high-resolution Landsat-5 TM data, in this paper, the optimal threshold of NDSI is obtained for identifying snow cover under different land cover types in the Tibetan Plateau. The results show that the optimal thresholds of NDSI are 0.33 and 0.4, respectively, under the type of grassland and sparse vegetation. The optimal threshold of NDSI is 0.47 under other land cover types. The snow cover determined by the NDSI threshold is accurately validated using Landsat 8 OLI data as "true value". The results show that the overall accuracy (OA), overestimated error (OE) and underestimated error (UE) of MODIS snow cover product based on new NDSI threshold are 87.88%, 5.20% and 6.87%, respectively. It is found that the OA, OE and UE based on traditional 0.4 threshold are 87.36%, 3.98% and 8.60%, respectively. It shows that NDSI threshold optimization under different land cover types can effectively improve the accuracy of snow cover in the Tibetan Plateau, especially in grassland areas with a large proportion of area, and the snow cover can be more accurately identified by NDSI threshold optimization.
  • WANG Xiaoru, TANG Zhiguang, WANG Jian, DEND Gang, WANG Xin, WEI Junfeng
    Journal of Glaciology and Geocryology. 2019, 41(5): 1173-1182. https://doi.org/10.7522/j.issn.1000-0240.2019.1164
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    Using the MODIS-derived 30 km grids (the number of grids is 744) snowline altitude at the end of ablation season and meteorological reanalysis data in the High Mountain Asia during 2001-2016 as the main data sources, the spatial distribution and heterogeneity of snowline altitude at the end of ablation season and their influencing factors are quantitatively analyzed based on Kriging interpolation, spatial variogram, regression analysis and correlation analysis methods. The following results are found:the spatial distribution of snowline altitude at the end of ablation season in the High Mountain Asia shows distinct spatial heterogeneity. The snowline altitude in the inner Tibet Plateau is relatively high (5 967 m a.s.l.) and shows small gradient of spatial variation; the lower values of snowline altitude (< 4 500 m) appear in the northern regions of the High Mountain Asia (the Altay Mts. and the Tianshan Mts.); the contour lines of snowline altitude are the densest in the west of the High Mountain Asia. On the 30 km grid scale, the snowline altitude at the end of ablation season in the High Mountain Asia has obvious spatial autocorrelation, with the spatial autocorrelation range of 1 550 km. The relative contribution ratios of the influences of latitude, longitude and altitude on snowline altitude at the end of ablation season are 60.5%, 2.6% and 36.9%, respectively, and the relative contribution ratios vary for different sub-regions. Summer mean air temperature is the dominant factor affecting the snowline altitude at the end of ablation season in the High Mountain Asia, and 45.6% of the grids are influenced by summer mean air temperature and distributed in all the subregions; the grids mainly affected by annual precipitation, accounted for about 18%, which are mainly distributed in the Karakoram Mountains and Pamir; only 10% of the grids are mainly affected by annual radiation (upward long wave flux at ground surface).
  • GUO Hui, CHEN Siyong, WANG Xiaoyan
    Journal of Glaciology and Geocryology. 2019, 41(5): 1183-1191. https://doi.org/10.7522/j.issn.1000-0240.2019.1180
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    Northeast China is one of the three major snow-covered areas in China, with forest coverage accounting for about 40% of the total area. Due to the influence of forest canopy, the standard model of snow cover provided by MODIS snow cover products (V6) is obviously underestimated. Based on this, the method of zoning modeling was adopted:in the forest area, the normalized difference forest snow cover index (NDFSI) was calculated, and the linear model between fraction of snow cover (FSC) and NDFSI and normalized difference vegetation index (NDVI) was established. In the non-forest areas, NDSI (normalized difference snow cover index) provided by MOD10A1 V6 was adopted to establish a linear relationship between pixel snow cover and NDSI and NDVI. In view of this situation, in this paper, the method of zonal modeling is adopted to calculate the NDFSI in forest areas; in the non-forest areas, the linear relationship between pixel snow cover and NDSI and NDVI is established by using NDSI provided by MOD10A1 V6. The fraction of snow cover extracted by Landsat 8 OLI was used to compare the estimation results of the zoning model with those of the standard algorithm model. The comparison shows that the root mean square error (RMSE) and the mean absolute error (MAE) in the process of estimating have greatly decreased as compared with the standard algorithm model, and this result has a more significant performance in the forest area. The coefficient of determination R2 calculated in this paper has also been greatly improved. Taking T1 forest areas image as an example, the mean square root error and the mean absolute error of the model are 0.246 and 0.055, respectively, while the two indexes of the standard algorithm model are 0.420 and 0.348, and the coefficients of determination of the algorithm model in this paper and the standard algorithm model are 0.675 and 0.641, respectively.
  • WEI Yarui, HAO Xiaohua, WANG Jian, LI Hongyi, ZHAO Hongyu, GAO Yang, SHAO Donghang, ZHONG Xinyue, LI Hongxing
    Journal of Glaciology and Geocryology. 2019, 41(5): 1192-1204. https://doi.org/10.7522/j.issn.1000-0240.2019.0525
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    Snow is the natural surface with high reflectivity on the earth, which plays an important role in the hydrological and energy balance in the middle and high latitudes. The change of black carbon and snow grain size in surface snow can significantly affect the albedo of snow, resulting in the change of solar radiation absorption by snow, and then produce feedback on regional climate change and hydrological cycle. Using remote sensing technology to quantitatively evaluate the black carbon and snow grain size of seasonal snow surface can obtain the variation of snow surface black carbon concentration and snow grain size in continuous system in time and space, which is also the input factor of many climate and hydrological models. In this paper, taking the northern Xinjiang of the main seasonal snow accumulation areas in China as the study area, based on the 3 (0.47 μm), 2(0.86 μm) and 5 (1.24 μm) bands of MODIS (Moderate Resolution Imaging Spectroradiometer) data, the snow surface black carbon concentration and snow grain size during the snow accumulation period from 2000 to 2018 are inversed by SGSP (Snow Grain Size and Pollution Amount) algorithm, and the accuracy of the inversion results is verified by the ground observation data. The temporal and spatial variation trend of snow surface black carbon concentration and snow grain size in northern Xinjiang was comprehensively analyzed. The results show that the SGSP algorithm can retrieve the black carbon concentration and snow grain size of snow surface at the same time, and the results show that the inversion results on pure snow pixels have good accuracy, and the average annual black carbon concentration and average annual snow grain size of snow surface in northern Xinjiang show a weak downward trend with the change of time from 2000 to 2018. Under the influence of geographical location and local pollution sources, the spatial distribution of snow black carbon concentration in northern Xinjiang is complex, the average black carbon concentration in the economic belt of the northern slope of Tianshan Mountain is the highest, the average black carbon concentration in Yili area is the lowest, the spatial distribution of snow grain size shows that the average snow grain size in Tacheng is the largest, and that in Yili is the smallest.
  • LI Zixuan, ZHAO Jiechen
    Journal of Glaciology and Geocryology. 2019, 41(5): 1205-1213. https://doi.org/10.7522/j.issn.1000-0240.2019.0324
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    Analysis of landfast ice in Arctic coastal areas is very important to provide a comprehensive understanding of the variations of Arctic sea ice, and to generate further basis data on the development and utilization of the Arctic shipping routes. Based on the weekly/biweekly sea ice analysis chart (2008-2018) released by the National Ice Center (NIC), we present a conversion and processing method to accurately extract the gridded data of the whole Arctic landfast ice distribution. The results showed that the average extent of Arctic landfast ice was (9.0±6.3)×105 km2 and has gradually decreased with an average rate of (-1.0±3.9)×103 km2·a-1. The landfast ice extent was the largest in April, with a multi-year mean of 1.6×106 km2. The extent from January to June in the Arctic winter was more than 1 million square kilometers, while almost no landfast ice in July-October, which was named Arctic summer. The MODIS images were used to verify the seven others in various months. The results showed that the average deviation in the end of freeze-up and the start of breakup was smaller. For example, the average deviation of the outer edge of the landfast ice was -0.8 km on March 12, 2012, and the deviation in the end of breakup was larger, such as the average deviation of the outer edge of the landfast ice was -9.4 km on September 14, 2009. However the verification error of all months was smaller than the grid size (25 km). Therefore, the method is considered to be credible, and the extracted gridded data may represent the true distribution of landfast ice.
  • CHEN Yizhuo, JI Qing, PANG Xiaoping
    Journal of Glaciology and Geocryology. 2019, 41(5): 1214-1220. https://doi.org/10.7522/j.issn.1000-0240.2019.0535
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    Long time sea ice thickness can be obtained via satellite altimetry at a large spatial scale. Compared to the Arctic, information of the Antarctic sea ice on thickness, especially in recent changes, is still scarce. We calculated Antarctic sea ice thickness from CryoSat-2 satellite altimeter data using the minimum elevation method and the static equilibrium equation model, and analyzed the spatio-temporal variation of Antarctic sea ice thickness from 2013 to 2018. The results show that the Antarctic sea ice thickness presents the trend of first rising and then falling. The annual mean sea ice thickness decreases rapidly during 2014-2017. Thicker ice is concentrated in the southwestern of the Weddell Sea, with the maximum occurring in July 2014 (6.27 m). The annual mean sea ice thickness reaches its lowest in 2017. This study can serve as a reference for further studying the relationship between sea ice and global change.
  • LI Shiweng, CHEN Tuo, ZHANG Wei, LIU Guangxiu
    Journal of Glaciology and Geocryology. 2019, 41(5): 1221-1234. https://doi.org/10.7522/j.issn.1000-0240.2019.1046
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    Cryosphere is an earth's sphere at subzero temperature on the earth. Microbes living in all the subspheres of cryosphere are unique members of biodiversity on the earth. Uncovering the rules of growth and proliferation, and origin and evolution of the microbes in cryosphere will greatly broaden the knowledge of bioscience and cryosphere science, but also provide valuable clues for understanding global change and exploring extraterrestrial life. The progress of microbiology of cryosphere will also benefit mankind. In this paper, we retrospect the research overview on the microbes in cryosphere and propose the concept of cryomicrobiology. The aim is to offer a new perspective for cryospheric science and microbiology.
  • GUI Juan, WANG Xufeng, LI Zongxing, ZOU Haiming, LI Aijun
    Journal of Glaciology and Geocryology. 2019, 41(5): 1235-1243. https://doi.org/10.7522/j.issn.1000-0240.2019.0530
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    under the background of ecological destruction, global climate change and the adjustment of planting structure in the Qilian Mountains, it is urgent to carry out long-term an effective monitoring and continuous research on the vegetation. Based on the resolution of 250 m of MODIS data in 2000-2017 and combining with climate data, using the Mann-Kendall non-parametric estimation model, as well as correlation analysis, the spatial and temporal variation characteristics of normalized difference vegetable index (NDVI) and vegetation in growing season of the Qilian Mountains and their correlation with climatic factors are analyzed. Also the impacts of human activities on vegetation are explored from both positive and negative aspects. The following conclusions can be drawn:(1) the average annual NDVI in the Qilian Mountains decreases gradually from east to west. NDVI first increase, and then decreases with the elevation rise; the maximum NDVI ranges between 2 700 and 2 900; (2) In the Qilian Mountains there is 0.6% of the total area having NDVI significantly decreasing and 33.6% of the total area having NDVI significantly increasing; the vegetation is showing a trend of overall improvement and local degradation; (3) The coverage of forest land, grassland and other land using area has increased by 0.0029, 0.0026 and 0.0004, respectively; the coverage of industrial and mining land has decreased by 0.0112, which reflect that the development of industry and mining has caused vegetation coverage decline; (4) The NDVI of planting and reforestation area have increased at the rate of 0.0455, while that of engineering implementation and mineral development area have decreased at the rate of 0.0125, indicating that human activities are one of the main factors leading to the change of vegetation community.
  • REN Liqing, RAN Youhua, REN Lixin, TAN Meibao
    Journal of Glaciology and Geocryology. 2019, 41(5): 1244-1253. https://doi.org/10.7522/j.issn.1000-0240.2019.0534
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    Vegetation is an important indicator of watershed ecological health, and vegetation landscape management is also an important part of integrated watershed management. In this paper, based on the Google Earth Engine (GEE) platform and the long time series MODIS reflectance and Normalized Difference Vegetation Index (NDVI) products and Landsat satellite images, the annual changes of natural vegetation and irrigated extent in Shiyang River basin (SRB) from 2001-2018 were monitored using an automatic classification method. Based on the ground-based data of precipitation, runoff and groundwater level, the temporal-spatial characteristics of natural vegetation and irrigation land change and their interaction with watershed water cycle variables include precipitation, runoff and groundwater level were analyzed. We found that the vegetation area in SRB increased with a rate of about 135 km2 per year from 2001 to 2018. Natural vegetation and irrigated land increased with a rate of 60.5 km2 and 74.6 km2 per year, respectively. Except for Jinchang area, the increase of vegetation is dominated by natural vegetation in other areas. Especially in Minqin area, groundwater level has been rising in recent years and natural vegetation has begun to recover due to more than ten years of continuous water diversion and effective control of cultivated land. However, this reduces the amount of water available in the middle reaches, and thus causing the increased ecological risks in Wuwei (Liangzhou District) and Yongchang County. In the future, the integrated management of river basins can be strengthened by comprehensive measures include irrigation land control, unified regulation of surface water and groundwater, optimization of industrial structure, and strengthening connectivity with the outside of the river basin. All of these are beneficial to improving the resilience of social ecosystems in SRB and enhance the ability of watershed sustainable development.
  • LIAN Xihong, QI Yuan, WANG Hongwei, ZHANG Jinlong, YANG Rui
    Journal of Glaciology and Geocryology. 2019, 41(5): 1254-1263. https://doi.org/10.7522/j.issn.1000-0240.2019.0531
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    Human activities change ecological patterns and changes, which in turn affect ecosystem services. Therefore, exploring the spatial pattern of ecosystem services under the influence of human activities is crucial for regional ecological security, sustainable development and human well-being. In this paper, the Qinghai Lake watershed is used as the research area. Based on the InVEST model, five ecosystem services such as water yield, water purification, habitat quality, soil conservation and carbon storage were calculated. The spatial autocorrelation, Interrelationships and spatial patterns under the influence of human activities were analyzed. The results show that:(1) The habitat quality was generally good, and the soil loss was small. There were significant spatial differences in carbon storage, which affected by vegetation cover. The load of nitrogen and phosphorus was high in agricultural ecosystem and urban ecosystem. The difference of water yield between lake area and mountain area was obvious; (2) Moran's I of water yield, carbon storage and habitat quality were 0.786, 0.742 and 0.705, respectively. Their spatial aggregation was the strongest, and the nitrogen load was the weakest; (3) The synergies were mainly between nitrogen load and phosphorus load, carbon storage and habitat quality, water yield and soil loss. The trade-offs were mainly between habitat quality and water yield and nitrogen load, carbon storage and water yield and soil loss. (4) Carbon storage, habitat quality and soil loss showed a decreasing trend with the enhancement of human activities. The load of nitrogen and phosphorus increased with the increase of human activities. Human activities affect water yield by altering impermeable surfaces. This study described the human activities by high-resolution remote sensing images, and the spatial pattern and aggregation degree of ecosystem services under the influence of human activities were discussed. The purpose of this paper is to provide a basis for scientific assessment of ecosystem service, ecological environment protection and sustainable development of watershed.
  • MA Xinggang, WANG Shijin, Qiongda, YANG Yuzheng, WEI Yanqiang, ZHOU Lanyue
    Journal of Glaciology and Geocryology. 2019, 41(5): 1264-1270. https://doi.org/10.7522/j.issn.1000-0240.2019.1174
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    Tourism has developed rapidly in glaciers, one of the most spectacular natural landscapes, in the past few decades. However, with global warming, glacier changing and glacier retreating have attracted widespread attention from governments and tourists around the world, the value of the glacier tourism is also rising. The glacier tourism resources in China are abundant with a golden future for tourism development. However, it was lack of scientific and rational development strategies in the past, glacier tourism development was slow and serious homogenization. It needs a good plan and to make the glacier tourism resources in China realize industrialized and large-scale development. Under this background, taking the Midui Glacier in Kangri Garpo Range, Tibet as an example, we analyzed the problems in the development process, and puts forward that the construction of infrastructure facilities and interpretation system should be accelerated constructing. The advantage of "the most beautiful glacier in China" should be highlighted in the development of glacier tourism in the future, and it is necessary to integrate the folk culture resources near Midui Glacier. We should stick to sustainable development strategies and create a characteristic brand of tourism culture. The purpose of this study is to enhance people's knowledge and protection awareness of glacier tourism, and to help local economy development rapidly. The purpose of this study is to enhance people's awareness of glacier tourism resources in China, form a sustainable development path of glacier tourism, and to promote the quality and efficiency of local economy.
  • YING Xue, WU Tonghua, SU Bo, ZHU Xiaofan, XIAO Yao
    Journal of Glaciology and Geocryology. 2019, 41(5): 1271-1280. https://doi.org/10.7522/j.issn.1000-0240.2019.0537
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    Cryosphere services refer to the benefits that humans can obtain directly or indirectly from the cryosphere, which is produced by the cryosphere processes and functions. They also provide an important material and cultural basis for human survival and development. With the development of the cryosphere science, people's understanding of the process and function of the cryosphere continues to deepen. At the same time, how cryosphere science serves regional sustainable development has also become an important research topic. In this context, the cryosphere service research began to receive the attention of the cryosphere science community. However, as one of the important contents of the research on cryosphere services, there is still a lack of systematic discussion on the assessment method of cryosphere services. In view of this, this study explores the evaluation methods of various cryosphere services from three dimensions:material quality method, value quantity method and energy value analysis method. Through the analysis of the applicable scope, basic use criteria and advantages and disadvantages of these three methods, in order to explore the most suitable methods for evaluating various cryosphere services, it can provide a reference for the later specific evaluation.