=Paper=
{{Paper
|id=Vol-2534/21_short_paper
|storemode=property
|title=Cartographic Modeling of Soil Temperature Fields for Middle Siberia Transect Based on Conjoint Analysis of Automated Ground-based and Satellite Temperature Data
|pdfUrl=https://ceur-ws.org/Vol-2534/21_short_paper.pdf
|volume=Vol-2534
|authors=Svetlana Ya. Kudryasheva,Alexander S. Chumbaev,Igor A. Pestunov,Yuriy N. Sinyavskiy,Dmitry L. Chubarov,Anna N. Bezborodova,Nicolay B. Ermakov
}}
==Cartographic Modeling of Soil Temperature Fields for Middle Siberia Transect Based on Conjoint Analysis of Automated Ground-based and Satellite Temperature Data==
https://ceur-ws.org/Vol-2534/21_short_paper.pdf
Cartographic Modeling of Soil Temperature Fields
for Middle Siberia Transect Based on Conjoint Analysis
of Automated Ground-based and Satellite Temperature Data1
Svetlana Ya. Kudryasheva1, Alexander S. Chumbaev1, Igor A. Pestunov2, Yuriy N. Sinyavskiy2,
Dmitry L. Chubarov2, Anna N. Bezborodova1, Nicolay B. Ermakov3
1
Institute of Soil Science and Agrochemistry SB RAS, Novosibirsk, Russia, sya55@mail.ru
2
Institute of Computational Technologies SB RAS, Novosibirsk, Russia, pestunov@ict.nsc.ru
3
Central Siberian Botanical Garden SB RAS, Novosibirsk, Russia, brunnera@mail.ru
Abstract. A series of cartographic models was created basing on the conjoint analysis of
quantitative indicators of the air and sols temperature regime, obtained by automated
ground and satellite temperature sensors. It reflects the characteristics of temperature
fields of typological units of soil-bioclimatic zonality for the Altai-Sayan region.
Key worlds: cartographic modeling; temperature fields; automated ground monitoring;
satellite data.
1 Introduction
The relevance of development of the geographic information concept for mapping the soil cover, soil properties
and regimes is presented in a large number of applications developed using geographic information systems and
technologies. The temperature regime is one of the most significant environmental factors, which together with the
hydrological regime characterizes the overall energy level of the formation and functioning of the soil cover. The
temperature field of soils is a set of temperature values at points in the spatial region, which according to the results of
studies obtained both in our country and abroad is considered as a leading factor in the structural and functional
organization of soil cover. For thematic mapping, soil properties are used that closely correlate with the
environmental characteristics and are due to the action of soil formation factors [1]. In the most complete form, the
factors determining the properties of soils at a certain point in the studied space are reflected in the SCORPAN model,
a soil spatially predicting function that assumes that the same combination of soil-forming factors-predictors
correspond to soils of similar genesis, and the boundaries of soil structures are due to changes in soil differentiation
factors. The most informative predictors are selected using the pedotransfer method approaches, which allow
calculating pedotransfer functions – communication equations that describe the functional relationships of basic soil
properties and characteristics of soil geographic space [2]. The main difference of this methodology is that, based on
the totality of the selected quantitative soil-ecological indicators, we can proceed to its taxonomic characterization.
This approach allows for the aggregate of homogeneous soil-forming predictor factors to spatially separate the areas
of soils and draw contour boundaries between them. Cartographic models of temperature fields obtained as a result of
a joint analysis of ground-based and satellite data are sufficiently informative with respect to the energy of soil-
forming processes and can be used to assess the thermal conditions of soils in poorly explored and inaccessible
territories of the Altai-Sayan region.
2 Study area and data
Testing of the methodological provisions for identifying the boundaries of temperature fields was carried out on
the example of typological units of the soil cover of the Altai-Sayan region, including a variety of steppes of the
Chulym-Yenisei and Minusinsk troughs, the Chuy, Kurai, Turan-Uyuk, Central Tuva, Ubsu-Nur basins and tundra-
steppe complexes Ukok Plateau. The key areas were selected taking into account the principles of landscape zoning,
which allows one to recognize, classify, and map landscape differentiating factors, landscape components, the
regional landscape structure as a whole, and its dynamic features. The method is based on a coupled analysis of
regional structures objectively reflected in satellite images and recorded on landscape-typological maps. Landsat 8/9
satellite images were used as information sources. Thematic soil and climate maps were used as auxiliary
Copyright © 2019 for this paper by its authors. Use permitted under Creative Commons License Attribution 4.0
International (CC BY 4.0).
maps for decoding satellite images. The intermountain basins of Khakassia and Tuva are located in the
eastern sector of the Altai-Sayan mountain region in the following sequence from north to south - Severo-
Minusinskaya, South Minusinskaya, Turano-Uyuk, Central Tuva and Ubsu-Nurskaya. The elevations of the bottoms
of the basins increase southward from 300 to 500 m above sea level in the basins of Khakassia and from 700 to 900 m
above sea level in the basins of Tuva. In the same direction, climate continentality increases – from the mildest
climatic conditions in the North Minusinsk to the most severe type of thermal regime in the Ubsu-Nur basin.
Distribution features and conditions for the formation of thermal conditions in the steppes of the left bank of the
Yenisei-Minusinsk depression (Khakassia) are associated with their location between the mountain structures of the
Kuznetsk Ala-Tau, East and West Sayan.
On the territory of Tuva, the Turano-Uyuk, Central Tuva and Ubsu-Nur steppe basins are clearly distinguished by
climate-forming factors and thermal conditions of soil formation. Within the boundaries of the Ukok highlands,
tundra-steppe complexes with a contrasting combination of mountain-steppe and mountain-tundra soils and
quantitative indicators of the soil climate stand out. The contrast of the climatic regimes of air and soils in the basins
of Khakassia is formed depending on the severity of the direction of moisture transfer, which in the eastern sector of
the Altai-Sayan mountain region has a western, alternating with a northwestern orientation (Table 1).
Climatic conditions, as a set of environmental factors, have a direct impact on the formation of the diversity of the
soil cover in the hollow steppes of Khakassia. In the regions of the Uzhuro-Kopiev and Shirin steppes, in which the
average annual air temperature is 1,3 °C, the frost-free period is 168 days and 𝛴𝑡 ∘ > 10∘ 𝐶 = 1573∘ southern and
ordinary chernozems prevail, occupying from 14 to 34% of the area.
In the Uybat steppe, located in close proximity to the eastern foothills of the Kuznetsk Ala-Tau, the average
annual air temperature is -1,1 °C, the frost-free period is 170 days and 𝛴𝑡 ∘ > 10∘ 𝐶 = 1630∘ . Therefore, the most
xerophilous core of the steppe vegetation is located here and low-fertile solonetzic soils are formed. In the Tuva
basins clearly differing in physical and geographical environmental conditions, annual and daily climate cycles,
temperature fields are distinguished, which can be considered as indicators of differences in the complex of climatic
conditions and the structural organization and functioning of the soil cover (Table 2).
Table 1. Air and soil temperature regime indicators by of the soil profile depths (cm) for Khakassia steppe basins.
Temperature Air temperature Soil temperature by the depths of the soil profile (cm), Т°С
indicators, Т°С Т°С on the soil surface 10 20 30 50
Uzuro-Kopievskaya meadow steppe, Kopievo (N54°56'19,6"; E89°52'47,1")
>10° 1461,5/89* 1674,5/100 1427,2/90 1400,7/90 1205,3/77 1202,9/83
>5° 1755,3/131 1917,3/133 1742,8/133 1711,8/132 1571,8/123 1508,5/126
>0° 1845,6/168 2026,7/176 1827,2/173 1819,3/183 1706,3/179 1631,8/177
<0° -1420,9/165 -1118,5/157 -1035,3/160 -879/150 -817,9/154 -642,8/156
average annual
1,3 2,7 2,4 2,8 2,7 3,0
temperature
Shirinsky lake-basin steppe, lake Tus (N54°45'17,2"; E89°57'17,9")
>10° 1558,8/90 1875,1/105 1707,9/100 1428,1/90 1359,9/87 1075,6/76
>5° 1859,6/130 2161/144 2020,7/141 1760,9/136 1721/135 1422,8/124
>0° 1974,5/169 2244,2/181 2127,2/185 1846/172 1842,5/183 1554,3/177
<0° -1544/164 -1168,2/152 -980/148 -973,7/161 -720,8/150 -639/156
average annual
1,3 3,2 3,4 2,6 3,4 2,7
temperature
Uybat plain-hilly solonetzic steppe, lake Ulug-Khol (N53°47'30,1"; E90°38'39,8")
>10° 1630,8/95 1785,7/105 1457,8/94 1363,7/90 1168,5/80 1091/79
>5° 1927,1/135 2059,4/142 1732,8/130 1674,9/132 1523/127 1407,8/121
>0° 2010,1/170 2118,6/164 1829,3/170 1767,4/169 1634,9/166 1553,8/174
<0° -1638,4/163 -1796,6/169 -1546/163 -1367,8/164 -1245,5/167 -1022,5/159
average annual
1,1 1,0 0,9 1,2 1,2 1,6
temperature
* the denominator is the number of days
Table 2. Air and soil temperature regime indicators by the soil profile depths (cm) for Tuva steppe basins.
Temperature Air, Soil temperature by the depths of the soil profile (cm), Т°С
indicators, temperature on the soil 10 20 30 50
Т°С Т°С surface
Turan-Uyuk basin, Turan (N52°08'18,8"; E93°49'25")
>10° 1572,8/95* 1754,1/96 1470,3/88 1284,9/82 908,9/70 1572,8/95*
>5° 1768,5/121 1951,4/124 1726/124 1536,5/116 1210,3/112 1768,5/121
>0° 1874/160 2026,5/152 1822,8/161 1660/163 1312,7/156 1874/160
<0° -2626,3/169 -2112,3/177 -843,8/168 -693,5/166 -270,3/171 -626,3/169
average annual -2,3 -0,3 -0,1 -0,1 0,1 -2,3
temperature
Ulug-Khem Basin, Kyzyl (N51°44'36,5"; E94°19'34,4")
>10° 2043,3/107 2327,3/120 1995,1/112 2151,3/121 1730,1/107 2043,3/107
>5° 2349,9/149 2603,5/156 2268,9/148 2458,9/163 2083,8/156 2349,9/149
>0° 2440,7/180 2672,4/183 2350,5/179 2515,4/192 2157/183 2440,7/180
<0° -2319,2/149 -1882,5/146 -752,3/150 -388,8/137 -1234/126 -319,2/149
average annual 0,4 2,4 1,8 3,4 2,8 0,4
temperature
Khemchik depression, Ak-Dovurak (N51°13'0,2"; E90°31'38")
>10° 2034,2/110 2484,9/125 2238,1/121 2155,7/118 2117,8/117 2034,2/110
>5° 2320,7/148 278,4/154 2450,5/149 2399,7/150 2376,7/151 2320,7/148
>0° 2383,6/174 2767/177 2511,3/175 2459,7/173 2440,3/170 2383,6/174
<0° -2586,9/155 -2199,8/152 -159,5/154 1994,9/156 -1844/159 -586,9/155
average annual -0,6 1,7 1,1 0,6 1,8 -0,6
temperature
Ubsu-Nur Basin, lake Tere-Khol (N50°15'23,4"; E95°0,2'32,3")
>10° 2207/125 2575/132 2400/133 2320/131 2226/128 2207/125
>5° 2407/151 2755/155 2522/150 2480/154 2448/158 2407/151
>0° 2461/169 2830/182 2603/179 2542/179 2496/179 2461/169
<0° -3114/172 -2035/159 -2024/162 -1884/162 -1613/162 -3114/172
average annual -1,9 2,3 1,7 1,9 2,6 -1,9
temperature
* the denominator is the number of days
The Turano-Uyuk Basin, located at an altitude of 700-900 m above sea level according to the main indicators of
the climatic regime – the average annual air temperature (-2.3°), the duration of the frost-free period (160 days) and
𝛴𝑡 ∘ > 10∘ 𝐶 = 1573∘ , it approaches the conditions of the arid steppe zone. Thermal conditions of the Ulug-
Khem and Khemchik hollows, the bottoms of which are 600-800 m above sea level, characterized by a higher average
annual air temperature (-0.4°), a longer frost-free period (180 days) and 𝛴𝑡 ∘ > 10∘ 𝐶 = 2043∘ . The Ubsu-Nur
basin is distinguished by a low atmospheric humidification and high heat resources of summer: average annual air
temperature (-1.9°), frost-free period – 169 days and 𝛴𝑡 ∘ > 10∘ 𝐶 = 2034∘ , which create a regime semi-desert
zone with chestnut soils and psammozems.
3 Ground-based automated monitoring of air and soils
Ground-based automated monitoring of air and soil was organized using a specialized temperature recorder DS-
1921G “Thermochron” taking into account indicators reflecting the genetic unity of the climate types of the Altai-
Sayan region. To fix the air temperature, an autonomous recorder was installed at a height of 2 m from the soil
surface under conditions excluding direct radiation exposure. The dynamics of temperature changes on the soil
surface and horizons of the soil profile was recorded during the year with an interval of 4 hours. As a result of the
observations, a large amount of evidence was obtained, which was used as the basis for calculating the thermal
resources of temperature fields and identifying their time trends [3].
4 Software and algorithms for MODIS data retrospective analysis, statistical processing
and visualization
Thematic processing of satellite images was carried out using the original nonparametric methods and
technologies for satellite images segmentation proposed by the authors, which allow taking into account both spectral
and spatial features, as well as ground-based observations [4-7].
For retrospective analysis, statistical processing and visualization of MODIS data were used the original software
and algorithmic tools created at ICT SB RAS, based on a new technology for access to the satellite data archive
implemented using the PostgreSQL DBMS with an additional module [4, 5]. This module is designed for direct
access to the file data archive without the need for preliminary copying and converting the data format for the DBMS.
It implements transparent mapping of the satellite image file archive into virtual database tables. The module allows
you to execute arbitrary SQL queries to the file archive data, while the query planner optimizes their execution based
on available metadata, and the algorithms used to perform the calculations provide for work with information
volumes exceeding the DBMS server RAM capacity. The developed system for extracting data from the satellite
imagery archive can be compared with such systems as NASA Giovanni, Google Earth Engine and the European
project TELEIOS. All are aimed at providing access to large volumes of satellite imagery. The created technology
surpasses the described systems in various aspects. There are no restrictions on the type of data queries, since
arbitrary SQL queries are supported. This system is designed to work with arbitrary spatial data without the need for
their preliminary transformation and preparation.
5 Cartographic modeling of the soil temperature fields heterogeneity
An interpretation of typological units of structural and functional organization for soil cover of steppe basins is
presented on the basis of a statistical analysis of the combination of boundaries and the information content of the soil
cover contours and the temperature field contours obtained from the analysis of satellite data of day and night
temperatures and the temperature difference of subtraction of two compiled series calculated for 16 year period
(2001-2016).
The possibility of cartographic modeling of the structural organization and functioning of the soil cover was
revealed using steppe basins of the Middle Siberian transect and tundra-steppe complexes of the high mountains of
the Altai-Sayan region as an example. The interpretation of typological units of the structural and functional
organization of the soil cover of the steppe basins of Khakassia is presented on the basis of a statistical analysis of the
combination of boundaries and the information content of the soil cover contours and temperature fields obtained by
analyzing satellite data of daytime, nighttime temperatures and temperature differences obtained by subtracting two
compiled series (Figure 1).
Figure 1. Cartographic models of the temperature fields of the steppes of Khakassia. A – daytime,
B – nighttime and C – temperature differences obtained by subtracting two compiled series. 1- temperature fields;
2 – statistical analysis of combining the boundaries of soil contours and temperature fields.
Figure 2. Cartographic models of the temperature fields of the steppes of Tuva. A – daytime;
B – nighttime and C – temperature differences obtained by subtracting two compiled series. 1 – temperature fields;
2 – statistical analysis of combining the boundaries of soil contours and temperature fields.
Figure 3. Cartographic models of the temperature fields of the tundra-steppe complexes of Ukok plateau.
A – daytime; B – nighttime and C – temperature differences obtained by subtracting two compiled series.
1 – temperature fields; 2 – statistical analysis of combining the boundaries of soil contours and temperature fields.
The obtained cartographic models give a clear idea of the boundaries of the temperature field contours of
typological units of the soil cover of Khakassia, the functioning of which is carried out in a wide range of
temperatures. They make it possible to get an idea of the thermal conditions of both large units of soil cover, such as
the Shirinskaya or Uybatskaya hollows, and occupying small areas – Koibalskaya or Sorokaozernaya, but having
independent environmental significance. Noteworthy are the significant difference in the allocation of areas of soil
contours and their temperature fields in the basins of dry (deserted) steppes, obtained on the basis of the analysis of
satellite data, both day and night temperatures. The spatial distribution of temperature fields, taking into account
current trends in thermal resources, can be used to adjust the contour boundaries of the structural units of the soil
cover.
The spatial distribution of temperature fields in the steppe basins of Tuva has a southwestern direction and is due
to the peculiarities of the macro relief. In the basins of Tuva, characterized by a high degree of diversity of
characteristics of the soil geographical space and aridization of the climate, the obtained cartographic models of
temperature fields can be used to identify spatial and temporal gradients of thermal resources at the scale of large and
local soil cover units (Figure 2).
Cartographic models of temperature fields are also informative for identifying the conditions of heat supply for
the formation and functioning of the tundra-steppe complexes of the Ukok highlands, for the soil cover of which
combinations of mountain-steppe and mountain-tundra soils are typical (Figure 3).
Temperature field models can be used to obtain additional information about natural complexes, the formation and
functioning of which is carried out under conditions of ultra-high or ultra-low temperatures.
In general, cartographic models of temperature fields obtained as a result of a joint analysis of terrestrial and
satellite data are sufficiently informative with respect to the energy of soil-forming processes and can be used to
assess the thermal conditions of soils in insufficiently studied and inaccessible territories of the Altai-Sayan region.
The novelty of the approach lies in the fact that cartographic models of soil temperature fields, created on the
basis of quantitative indicators of the temperature regime, have sufficient information content to establish
relationships with other characteristics of environmental objects and to solve the problem of distinguishing the
boundaries of temperature fields of typological units of soil cover.
Acknowledgements. The authors are grateful for the financial support of the RFBR project
No 18-04-00633-a.
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