Monitoring and comparing NDSI changes using MODIS and ETM+ sensor data to estimate snow cover in North Karun Basin

Document Type : Research/Original/Regular Article

Authors

1 Assistant Professor/ Soil and Water Research Department, Chaharmahal and Bakhtiari Agricultural and Natural Resources Research Center, AREEO, Shahrekord, Iran.

2 Expert of Farrokhshahr Agricultural Meteorological Research Center/ Shahrekord, Iran

Abstract

Introduction
North Karun Basin is one of the snow-covered regions of Iran and its snowfall has a great role in the water supply situation in the central and southern regions of the country. In this research, an attempt has been made to investigate the changes in the snow-covered surface in the study basin. Access to this information in high and impassable areas is possible only with the help of remote sensing techniques. The MODIS sensor has multiple spectral bands, but the ETM+ sensor has a better spatial resolution. The purpose of this study is to monitor, compare and map snow-covered areas by MODIS and ETM+ data in the northern part of the Karun Basin.
Materials and Methods
The research has been conducted in the northern part of Karun Basin, as one of the snowy areas in Iran. This area is geographically between 31° 19' 9'' to 31° 39' 17'' northern latitude and 49° 33' 56'' to 51° 54' 23'' eastern longitude. The study basin is over 14802 square kilometers, about 90% of Chaharmahal and Bakhtiari Province and 23% of Karun Basin. The height of the study area is changing between 800 m at Karun No. 4 dam to 4440 m at the Peak of Zard Kooh Mountain. The satellite data included MODIS and ETM+ sensors over a period of 15 years (2000 to 2015) used to calculate NDSI. The satellite pass-times were at Julian day number 360, 333, 365, 355, 360, 363, 331, 350, 336, 355, 342, 345, 363, 334 and 1.
Results and Discussion
The minimum and maximum snow-covered areas produced by MODIS in 2010 and 2013 were 107,295 and 1,364,118 ha, respectively, and for ETM+ sensor, were 128,758 and 1,090,580 ha, in 2010 and 2006, respectively. The snow-covered areas estimated by MODIS in 14 dates were more than the corresponding values for ETM+. The exception was 2011 when the snow-covered area in the ETM+ was greater than MODIS (3067 ha or 1.36%). Based on the results in 15 years, the MODIS sensor overestimated the snow-covered area equivalent to 26.95% compared to ETM+. In a small snow-covered area, deviation from the 1:1 line was small but, by increasing snow-covered area, deviation increased. The overall difference in snow pixels in the 15 years between the two sensors was 26.95%. As MODIS pixels are 500 by 500 m, and ETM+ pixels are 30 by 30 m, the size of the pixels in ETM+ resized to 500 m by resampling method in which to use same pixel size for another comparison. After resampling, the slope of the regression line slightly dropped. However, there are no-significant differences. Using data from MODIS and ETM+ sensors had a good performance to monitor spatio-temporal and map snow-covered surfaces in North Karun Basin.
Conclusion
Due to spatio-temporal frequency in obtaining MODIS imageries via internet freely in temporal resolution of eight-days and one-day, and also at very wide area coverage, short-time monitoring is possible for hydrological studies, forecasting and flood warning. On the other hand, the ability and better spatial resolution of ETM+, small snowy fields could be estimated and mapped better than MODIS. Although it may be need to mosaic several ETM+ imageries to cover wide areas. However, paying attention to geographical characteristics and time of the study area, end user decides to choose one or both sensor data.

Keywords

References

Afifi, M.E. (2021). Investigation of changes in snow cover and determination of snowmelt line in mountainous areas using MODIS images and NDSI index (Case study of Zagros Glaciers). Geography and Environmental Studies, 10(38), 25-36 (in Persian).
Barton, J.S., Hall, D.K., & Riggs, G.A. (2000). Remote sensing of fractional snow cover using Moderate Resolution Imaging Spectroradiometer (MODIS) data. Proceedings of the 57th Eastern Snow Conference, Syracuse, New York, USA.
Cline, D.W. (1997). Snow surface energy exchanges and snowmelt at a continental, midlatitude Alpine site. Water Resources Research, 33, 689.
Crawford, C.J. (2015). MODIS Terra Collection 6 fractional snow cover validation in mountainous terrain during spring snowmelt using Landsat TM and ETM+. Hydrological Processes, 29(1), 128-138.
Custodio, E., Cabrera, M.C., Poncela, R., Puga, L.O., Skupien, E., & del Villar, A. (2016). Groundwater intensive exploitation and mining in Gran Canaria and Tenerife, Canary Islands, Spain: Hydrogeological, environmental, economic and social aspects. Science of The Total Environment, 557-558, 425-437.
Dini, G.R., Ziaeian Firozabadi, P., Ali Mohammadi Sarab, A., & Dadashi Khanghah, S. (2008). GIS-based snow mapping in central Alborzmountain chain using MODIS and AVHRR data. Iran-Water Resources Research, 3(3), 1-8 (in Persian).
Donmez, C., Berberoglu, S., Cicekli, S.Y., Cilek, A., & Arslan, A.N. (2021). Mapping snow cover using landsat data: Toward a fine-resolution water-resistant snow index. Meteorology and Atmospheric Physics, 133(2), 281-294.
Dozier, J. (1989). Spectral signature of alpine snow cover from the landsat thematic mapper. Remote Sensing of Environment, 28, 9-22.
Drewry, D. (1986). Remote sensing for polar regions - remote sensing ice and snow. D.K. Hall and J. Martinec 1985. London, New York, Chapman and Hall. 189 p, illustrated, hard cover. ISBN 0412259109. Polar Record, 23(143), 213-214.
Faizizadeh, B. (2019). A comparative evaluation of pixel-based and object-oriented processing techniques, used for the classification of Aster Satellite imageries and extracting agricultural and orchard maps in the Eastern Margin of Urmia Lake. Scientific- Research Quarterly of Geographical Data (SEPEHR), 28(109), 167-183 (in Persian).
Gerland, S., Winther, J.G., Ørbæk, J.B., Liston, G.E., Øritsland, N.A., Blanco, A., & Ivanov, B. (1999). Physical and optical properties of snow covering Arctic tundra on Svalbard. Hydrological Processes, 13(14-15), 2331-2343.
Ghanbarpour, M.R., Mohsen Saravi, M., Saghafian, B., Ahmadi, H., & Abbaspour, K. (2005). An evaluation of regions effective in accumulation and persistence of snow cover and snowmelt contribution in runoff. Iranian Journal of Resources, 58(3), 503-515 (in Persian).
Ghorbanizadeh Kharazi, H., Sedghi, H., Saghafian, B., & Porhemat, J. (2007). The study on the effect of climate change on the peak time of snowmelt runoff. Plant and Ecosystem, 3(11), 38-50 (in Persian).
Haghizadeh, A., Yousefi, H., Yarahmadi, Y., & Kiyani, A. (2020). Simulation of climate change impact on snowmelt runoff (Case study: Sarab Seyed Ali Watershed-Lorestan). Water and Irrigation Management, 10(1), 101-112 (in Persian).
Hall, D., Foster, J., Verbyla, D., Klein, A., & Benson, C. (1998). Assessment of snow-cover mapping accuracy in a variety of vegetation-cover densities in central Alaska. Remote Sensing of Environment, 66(2), 129-137.
Hall, D., Riggs, G., Salomonson, V., & Scharfen, G. R. (2000). Earth Observing System (EOS) Moderate Resolution Imaging Spectroradiometer (MODIS) global snow-cover maps. IAHS-AISH publication, 55-60.
Hall, D.K., Riggs, G.A., Salomonson, V.V., Barton, J., Casey, K., Chien, J., DiGirolamo, N., Klein, A., Powell, H., & Tait, A. (2001). Algorithm theoretical basis document (ATBD) for the MODIS snow and sea ice-mapping algorithms. Nasa Gsfc, 45, 15-16.
Hall, D.K., Riggs, G.A., Salomonson, V.V., DiGirolamo, N.E., & Bayr, K.J. (2002). MODIS snow-cover products. Remote Sensing of Environment, 83(1-2), 181-194.
Kadkhodaei, S., Jahanbakhsh Asl, S., & Valizadeh Kamran, K. (2020). The estimation of snowmelt runoff using SRM model (case study: Sahzab Catchment). Geography and Planning, 24(71), 319-337 (in Persian).
Khosravi, M., Tavousi, T., Raeespour, K., & Omidi Ghaleh mohammadi, M. (2017). A survey on snow cover variation in Mount Zardkooh-Bakhtyare using remote sensing (R.S). Hydrogeomorphology, 4(12), 25-44.
Larney, F., & Timmerman, L.J. (2001). An Introduction to Wind Erosion Control, Alberta Government, Alberta.
Manickam, S., & Barros, A. (2020). Parsing synthetic aperture radar measurements of snow in complex terrain: scaling behaviour and sensitivity to snow wetness and landcover. Remote Sensing, 12(3), 483.
Marsh, P., & Woo, M. (1985). Meltwater Movement in Natural Heterogeneous Snow Covers. Water Resources Research, 21, 1710-1716.
Mashayekhi, T. (1990). Application of snow hydrology in water resources surveys. Report of the Office of Water Resources Surveys, Department of Surface Water (in Persian).
Mir Yaghoobzadeh, M.H., & Ghanbarpour, M.R. (2010). Investigation to MODIS snow cover maps usage in snowmelt runoff modelling (Case study: Karaj dam basin). GEOSCIENCES, 19(76), 141-148 (in Persian).
Mohammadi Farsani, Sh. (1998). Investigation and forecasting of Zayandehrood River Basin during snowmelt. M.Sc Thesis, Shiraz University, Shiraz, Iran (in Persian).
Najafzadeh, R., Abrishamchi, A., Tajrishi, M., & Taheri Shahraeeni, H. (2005). Stream Flow with snowmelt runoff modeling using RS and GIS (Case study: Pelasjan Sub-basin). Journal of Water and Wastewater, 15(4), 2-11 (in Persian).
Nolin, A., & Dozier, J. (2000). A Hyperspectral Method for Remotely Sensing the Grain Size of Snow. Remote Sensing of Environment, 74, 207-216.
Parajka, J., Holko, L., & Kostka, Z. (2001). Distributed modelling of snow water equivalent – Coupling a snow accummulation and melt model and GIS. Institute of Hydrology, Slovak Academy of Sciences, 14, 86-102.
Porhamat, J. (2002). Distribution model of runoff from snowmelt using remote sensing data. PhD Thesis, Science and Research Branch of Azad University, Tehran, Iran (in Persian).
Porhemat, J., & Saghafian, B. (2007). Evaluation of spatial resolution of satellite data on snow cover estimates. Iranian Journal of Natural Resources, 60(2), 383-395 (in Persian).
Raigani, B., Khajeh Aldin, S.J.A.D., Soltani Koupaei, S., & Barati, S. (2008a). Analysis of MODIS snow-cover map changes during missing data period. Water And Soil Science (Journal of Science and Technology of Agriculture And Natural Resources), 12(44), 315-332 (in Persian).
Raigani, B., Soltani Koupaei, S., Khajeh Aldin, S.J.A.D., & Barati, S. (2008b). Using MODIS images and NDSI index for preparation snow cover maps. Iranian Journal of Natural Resources, 61(3), 525-536 (in Persian).
Rango, A., Walker, A.E., & Goodison, B.E. (2000). Snow and Ice. Pp. 239-270, In: G.A. Schultz & E.T. Engman (Eds.), Remote Sensing in Hydrology and Water Management, Springer Berlin Heidelberg.
Rasouli, A.A., & Adhami, S. (2007). Estimation of snow water equivalent by processing of modis satellite imageries. Geography and Development, 5(10), 23-36 (in Persian).
Rittger, K., Krock, M., Kleiber, W., Bair, E.H., Brodzik, M.J., Stephenson, T.R., Rajagopalan, B., Bormann, K.J., & Painter, T.H. (2021). Multi-sensor fusion using random forests for daily fractional snow cover at 30 m. Remote Sensing of Environment, 264, 112608.
Schneebeli, M. (2002). The importance of the microstructure of snow in nature and engineering. Pp. 87–93, In: Brebbia, C.A., L.J. Sucharov and P. Pascolo, eds. Design and nature: comparing design in nature with science and engineering, Southampton, etc., WIT press. 
Sharifi, M.R., Akhound Ali, A.M., Porhemat, J., & Mohammadi, J. (2008). Effect of elevation, slope and aspect on snow depth at Samsami Basin. Iran-Water Resources Research, 3(9), 69-79 (in Persian).
Shayan, S., Yamani, M., & Yadegari, M. (2017). Zoning of the land subsidence in the Hamedan Qarachai Watershed. Hydrogeomorphology, 3(9), 139-158.
Vafakhah, M., Mohseni Saravi, M., Mahdavi, M., & Alavipanah, S.K. (2011). Comparison of snow cover area (SCA) in NOAA and MODIS images (A case study: Taleghsn Watershed). Watershed Management Researches (Pajouhesh-Va-Sazandegi), 24(3), 80-94 (in Persian).
Warren, S.G. (1982). Optical properties of snow. Reviews of Geophysics, 20(1), 67-89.
Wiscombe, W.J., & Warren, S.G. (1980). A Model for the Spectral Albedo of Snow. I: Pure Snow. Journal of Atmospheric Sciences, 37(12), 2712-2733.
Zeynali, B., Ghale, E., & Safari, S. (2021). Extraction of snow-covered area of Sabalan Mountain using Landsat satellite images by object-oriented classification method. Hydrogeomorphology, 8(26), 79-97 (in Persian).
Zhang, Y., Cao, T., Kan, X., Wang, J., & Tian, W. (2017). Spatial and temporal variation analysis of snow cover using MODIS over Qinghai-Tibetan Plateau during 2003–2014. Journal of the Indian Society of Remote Sensing, 45(5), 887-897.
Water and Soil Management and Modelling
Volume 1, Issue 4
2021
Pages 68-82

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History

  • Receive Date: 25 August 2021
  • Revise Date: 24 September 2021
  • Accept Date: 24 September 2021

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