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  <front>
    <journal-meta />
    <article-meta>
      <title-group>
        <article-title>Spatio-temporal analysis through remote sensing and GIS in Moscow region, Russia</article-title>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author">
          <string-name>Komal Choudhary</string-name>
          <xref ref-type="aff" rid="aff3">3</xref>
        </contrib>
        <contrib contrib-type="author">
          <string-name>M.S. Boori</string-name>
          <xref ref-type="aff" rid="aff0">0</xref>
          <xref ref-type="aff" rid="aff1">1</xref>
          <xref ref-type="aff" rid="aff3">3</xref>
        </contrib>
        <contrib contrib-type="author">
          <string-name>A. Kupriyanov</string-name>
          <xref ref-type="aff" rid="aff2">2</xref>
          <xref ref-type="aff" rid="aff3">3</xref>
        </contrib>
        <aff id="aff0">
          <label>0</label>
          <institution>American Sentinel University</institution>
          ,
          <addr-line>2260 South Xanadu Way, Suite 310, Aurora, Colorado 80014</addr-line>
          ,
          <country country="US">USA</country>
        </aff>
        <aff id="aff1">
          <label>1</label>
          <institution>Bonn University</institution>
          ,
          <addr-line>Meckenheimer Allee 166, D-53115 Bonn</addr-line>
          ,
          <country country="DE">Germany</country>
        </aff>
        <aff id="aff2">
          <label>2</label>
          <institution>Image Processing Systems Institute - Branch of the Federal Scientific Research Centre “Crystallography and Photonics” of Russian Academy of Sciences</institution>
          ,
          <addr-line>151 Molodogvardeyskaya st., 443001, Samara</addr-line>
          ,
          <country country="RU">Russia</country>
        </aff>
        <aff id="aff3">
          <label>3</label>
          <institution>Samara National Research University</institution>
          ,
          <addr-line>34 Moskovskoe Shosse, 443086, Samara</addr-line>
          ,
          <country country="RU">Russia</country>
        </aff>
      </contrib-group>
      <pub-date>
        <year>2017</year>
      </pub-date>
      <fpage>42</fpage>
      <lpage>46</lpage>
      <abstract>
        <p>Spatio-temporal analysis is a process for city development with growing population and economy for better implementation of planning policies with advance technology. In this research work, three dates (1995, 2005 &amp; 2016) satellite images were used to mapping and monitoring of Moscow region, Russia. This study focuses on the further classification of the study area into different categories on the basis of use and association by implementing a rule-based classification system on remotely sensed data. This research provides useful and up-to-date information to local land use planners, managers and policy-makers to step up towards sustainable development in Moscow region, Russia.</p>
      </abstract>
      <kwd-group>
        <kwd>Spatio-temporal</kwd>
        <kwd>land use/cover</kwd>
        <kwd>remote sensing</kwd>
        <kwd>GIS</kwd>
      </kwd-group>
    </article-meta>
  </front>
  <body>
    <sec id="sec-1">
      <title>1. Introduction</title>
    </sec>
    <sec id="sec-2">
      <title>2. Study area</title>
      <p>Moscow region is the one of the most densely populated regions in the country and is the second most populated federal
region. The Oblast has no official administrative center, it is public authorities are located in Moscow and across other locations
in the oblast. As of the 2010 Census, its population was 7,095,120 and 7,231,068 recorded in the 2015 Census. The latitude of
the city is 55° 45’ 7” N and longitude is 37° 36’ 56" E. The region is highly industrialized, such as metallurgy, oil refining,
mechanical engineering, food, energy and chemical industries [7].</p>
      <p>The climate of Moscow region is humid continental, short but warm summers and long cold winters. The average temperature
is 3.5 °C (38.3 °F) to 5.5 °C (41.9 °F).The coldest months are January and February average temperature of −9 °C (16 °F) in the
west and −12 °C (10 °F) in the east. The minimum temperature is −54 °C (−65 °F). Here are more than three hundred rivers in
Moscow region. The first largest river is Volga, most river belong to the basin of the Volga. Which itself only crosses a small
part in the north of Moscow Oblast. They are mostly fed by melting snow and the flood falls on April-May. The water level is
low in summer and increases only with heavy rain. The river freezes over from late November until April.</p>
    </sec>
    <sec id="sec-3">
      <title>3. Material and methods</title>
      <p>
        The Landsat program is a series of Earth-observing satellite mission jointly managed by NASA and the U.S. geological survey
[8]. The first Landsat satellite was launched in 1972 and the most recent one Landsat 8 was launched on February 11, 2013.
Data from Landsat 8 has eight spectral bands with spatial resolutions ranging from 15 to 60 m. The Landsat satellite data of
1995, 2005
        <xref ref-type="bibr" rid="ref2 ref9">and 2016</xref>
        have been used in this study with a spatial resolution of 30 m. The satellite data were checked completely
before classification into land use groups [9-10]. There are many techniques available for detecting and recording differences,
      </p>
      <p>Image Processing, Geoinformation Technology and Information Security / Komal Choudhary, M.S. Boori, A. Kupriyanov
ratios and correlation. The data used in this paper were divided into two categories first satellite data and second ancillary data.
Satellite data for the other hand consisted of multi- spectral data acquired by Landsat satellite provided by USGS gloves [11].
Ancillary data include ground truth data for the land use/cover classes and topographic maps. Spectral charts were prepared to
distinguish and find out the difference in pixel values of different land use/cover classes in different bands. Primary land use
classes were defined, such as agriculture, barren land, forest, settlements, scrubland, water body and wetland. The land use
classes are defined in Table 1.
3.1 Database preparation</p>
      <p>
        Any study of land use changes will involve the analysis of both conventional and remotely sensed data. Conventional data is
more accurate and site specific, but its collection is time consuming, manpower hungry and difficult to extrapolate over a larger
area. Remotely sensed data, on the other hand, has several advantages due to its repetitive and synoptic coverage of large and
inaccessible areas in a quick and economical fashion. In the present study both conventional and remotely sensed data were
used. The specific satellite images used were Landsat ETM+ (Enhanced Thematic Mapper plus) for 1995 and 2005, Landsat
OLI (Oper
        <xref ref-type="bibr" rid="ref2">ational Land Imager) for 2016</xref>
        , an image captured by a different type of sensors at a resolution of 30m were used for
land use/cover classification. These data sets were imported in ArcGIS 10.2 software. Satellite images were making by
processing software to create composites. A Trimble hand-held GPS with an accuracy of 10 meters was used to map and collect
the coordinates of important land use features during pre- and post-classification field visits to the study area in order to prepare
land-use and land-cover maps.
3.2 Image classification
      </p>
      <p>Land cover classes are typically mapped from digital remotely sensed data using some sort of supervised, digital image
classification. The overall objective of the image classification procedure is to automatically categorize all pixels in an image
into land-cover classes or themes and the maximum likelihood classifier quantitatively evaluates both the variance and
covariance of the category’s spectral response patterns whenever it classifies an unknown pixel. This is why it is considered to
be one of the most accurate classifiers - it is based on statistical parameters. Supervised classification was performed here using
ground checkpoints and digital topographic maps
3.3 Land use/cover change detection and analysis</p>
      <p>Land use maps shows in figures 2, were prepared using Landsat data. The accuracy of these classified maps was checked
using the GIS tools. The accuracy for these periods is 90% respectively. There is a big change in land use during this time
period. To order increase the accuracy of the land use mapping of the two images, ancillary data, and the result of visual</p>
      <p>
        Image Processing, Geoinformation Technology and Information Security / Komal Choudhary, M.S. Boori, A. Kupriyanov
interpretation was integrated with the classification results using Arc GIS [12, 13]. The classification of imagery from each
individual year, a multi-date, post-classification comparison, change-detection algorithm was used to determine changes during
two intervals from 1995-
        <xref ref-type="bibr" rid="ref6">2005 and 2005</xref>
        -2016. This is perhaps the most common approach to change detection. The
postclassification approach provides ‘from-to’ change information which facilitates easy calculation and mapping of the kinds of
landscape transformations that have occurred [14]. Accuracy assessment was then carried out at 85 points, 65 from the field data
and 20 from existing topographic maps and the land cover map. Specification of these 85 points used a stratified, random
method so that all of the different land-cover classes would be represented. In order to increase the accuracy of the land-cover
mapping of the two images, ancillary data as well as the result of visual interpretation was integrated with the classification
results using GIS [14]. The aim of this was to improve the classification accuracy of the classified image.
02/1995
02/2016
02/2005
Legend
Lulc Classes
      </p>
      <p>Agriculture
Barren land
Forest
Scrubland
Settlements
Water body</p>
      <p>Wetland
0 20 40
80
120
160</p>
      <p>Kilometers</p>
    </sec>
    <sec id="sec-4">
      <title>Results and Discussion</title>
      <p>
        There is a big change in land use during this time period, as show in the graphical representation of the data in figure 2.
Classification maps were generated for all of the sixteen years shown in figure and the individual class area and change statistics
are summarizes in table 1. In 1995 the urban area covered 3898.31 km2 (8.34 %), but by 2005 it had increased to approximately
4361.75 km2 (9.33 %)
        <xref ref-type="bibr" rid="ref2 ref9">and in 2016</xref>
        had increased to 5852.00 km2 (12.51). The agricultural area first half decreased from
13673.51 km2 (29.24 %) in 1995 to 6504.00 km2 (13.91 %) by 2005 and then increased to 13403.62 km2 (28.66 %) by 2016.
The forest area increased from 1995 21135.18 km2 (45.19 %) to 24671.31 km2 (52.75 %) by 2005 and then it was decreased
      </p>
      <p>
        Image Processing, Geoinformation Technology and Information Security / Komal Choudhary, M.S. Boori,
        <xref ref-type="bibr" rid="ref2">A. Kupriyanov
from 2016</xref>
        to 19896.64 km2 (42.54 %). The barren land area was 3802.63 km2 (8.13 %) in 1995, in 2005 had increased 4717.74
km2 (10.09 %) and then it had decreased 2993.18 km2 (6.40 %) by 2016.
      </p>
      <p>All the urban categories increased continuously, with the urban area increasing by 1953.69 km2 (4.17%) since 1995. Results
show that forest area has been most dominant class in the study area for all three dates. The land use transition during the
19952016 periods is shows in table 2.</p>
      <p>Table 2 shows both positive and negative land use/cover changes in the study area from 1995 to 2005, the major change was
in agriculture and forest area. Forest was increase 3,536.13 km2 (7.56) and agriculture was decrease 7169.51 km2 (15.33%) of
the total study area due to hares climatic conditions. From 2005 to 2016 total agriculture area was increase from 6,899.62 km2.
In the same time period other classes such as barren land, scrubland, settlements, water body and wetland increase respectively.
From 2005 to 2016 total agricultural area was increase from 6,899.62 km2and other classes settlements and waterbody were
increased.</p>
      <p>Class
Agriculture
Barren land
Forest
Scrubland
Settlements
Water body
Wetland
Total</p>
      <p>Total 13549.18 2976.32 19791.85 3484.42 5965.35 451.06 549.92 46768.12</p>
      <p>
        The results show that from1995 to 2005, 3820.91 km2 agriculture areas was stable but 990.98 km2 areas converted from forest
to agriculture (table 3). In the same time period 15982.20 km2 forest areas was stable but 1662.39 km2 wetland area was
encroached by forest. Maximum stable class was water body, where 293.26 km2 areas were stable from 1995 to
        <xref ref-type="bibr" rid="ref6">2005. In second
half from 2005</xref>
        to 2016 3926.40 km2 agriculture area was stable and 2711.65 km2 barren land, 4401.14 km2 forest and 1129.97
km2 scrubland area converted into agriculture land due to increase of market demand. In this time period there is a not a big
change in wetland and maximum bare land area 276.12 km2was stable. Scrubland 906.20 km2 and wetland 1238.38 km2 area
was converted into forest area which shows governmental protection from 2005 to 2016. Since 2005 to 2016, 2354.45 km2
settlements area was stable but 1798.50 km2 forest area was converted into settlements. In the second half again water body area
was highly stable area around 326.62 km2.
      </p>
      <p>As show by our study, land –cover change is mainly driven by the expansion of socio-economic activities. The increase of
agricultural areas, if poorly managed has impacts above those previously mentioned changes in the soil water cycle, nutrient</p>
      <p>Image Processing, Geoinformation Technology and Information Security / Komal Choudhary, M.S. Boori, A. Kupriyanov
depletion and an increased risk of soil erosion and land degradation even though the expansion of croplands leads to a growth in
agricultural outputs like food and fibers to positively impact on the country’s economy and human well- being.
As well as the huge increased in agricultural area there has also been a considerable increase in urban settlements. Such changes
require rapid adjustments to land management in order to avoid crises in food. From a socio-economic point of view this means
not only a loss of ecosystem services, but also a decline of earn money and cultural values, not to mention a subsequent
reduction of income from tourism. A consequence of this is to make protected areas some of the few remaining zones where fuel
wood, rich pastures and game resources are left and so they attract more and more legal activities.</p>
    </sec>
    <sec id="sec-5">
      <title>5. Conclusion</title>
      <p>In this new period of globalization cities should have quality infrastructure, energy and environment condition to sustain
growth and attract foreign investment. The planning authorities should adopt new technologies such as remote sensing and GIS
to address these issues. Remote Sensing and GIS are adequate of providing the necessary information and intelligence for
planning proposal. In this research remote sensing and GIS have been unified to exhibit the changes in urban development and
its future growth trends. This study focus on discover the expansion of the urban area of Moscow region. A large percentage of
barren land was transformed into urban area during the study period. The urban growth shows maximum detail on the outskirts
of the region. This expansion also indicates of industrial growths. Only remote sensing data can provide complete spatial
information for the efficient assignment of urban growth in developing countries over the time period.</p>
    </sec>
    <sec id="sec-6">
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