Dust storms in Kazakhstan: Frequency and division

Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite i...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Issanova, Gulnura [verfasserIn] Abuduwaili, Jilili Kaldybayev, Azamat Semenov, Oleg Dedova, Tatiana

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2015

Schlagwörter:	Dust storms soil texture deserts Kazakhstan Central Asia

Anmerkung:	© Geological Society of India 2015

Übergeordnetes Werk:	Enthalten in: Journal of the Geological Society of India - New Delhi : Springer India, 1959, 85(2015), 3 vom: März, Seite 348-358
Übergeordnetes Werk:	volume:85 ; year:2015 ; number:3 ; month:03 ; pages:348-358

Links:	Volltext

DOI / URN:	10.1007/s12594-015-0224-5

Katalog-ID:	SPR026211505

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912			\|a GBV_ILN_187
912			\|a GBV_ILN_213
912			\|a GBV_ILN_224
912			\|a GBV_ILN_230
912			\|a GBV_ILN_250
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912			\|a GBV_ILN_602
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912			\|a GBV_ILN_2107
912			\|a GBV_ILN_2108
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matchkey_str	article:09746889:2015----::uttrsnaahtnrqec
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publishDate	2015
allfields	10.1007/s12594-015-0224-5 doi (DE-627)SPR026211505 (SPR)s12594-015-0224-5-e DE-627 ger DE-627 rakwb eng Issanova, Gulnura verfasserin aut Dust storms in Kazakhstan: Frequency and division 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. Dust storms (dpeaa)DE-He213 soil texture (dpeaa)DE-He213 deserts (dpeaa)DE-He213 Kazakhstan (dpeaa)DE-He213 Central Asia (dpeaa)DE-He213 Abuduwaili, Jilili aut Kaldybayev, Azamat aut Semenov, Oleg aut Dedova, Tatiana aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 85(2015), 3 vom: März, Seite 348-358 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:85 year:2015 number:3 month:03 pages:348-358 https://dx.doi.org/10.1007/s12594-015-0224-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2015 3 03 348-358
spelling	10.1007/s12594-015-0224-5 doi (DE-627)SPR026211505 (SPR)s12594-015-0224-5-e DE-627 ger DE-627 rakwb eng Issanova, Gulnura verfasserin aut Dust storms in Kazakhstan: Frequency and division 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. Dust storms (dpeaa)DE-He213 soil texture (dpeaa)DE-He213 deserts (dpeaa)DE-He213 Kazakhstan (dpeaa)DE-He213 Central Asia (dpeaa)DE-He213 Abuduwaili, Jilili aut Kaldybayev, Azamat aut Semenov, Oleg aut Dedova, Tatiana aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 85(2015), 3 vom: März, Seite 348-358 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:85 year:2015 number:3 month:03 pages:348-358 https://dx.doi.org/10.1007/s12594-015-0224-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2015 3 03 348-358
allfields_unstemmed	10.1007/s12594-015-0224-5 doi (DE-627)SPR026211505 (SPR)s12594-015-0224-5-e DE-627 ger DE-627 rakwb eng Issanova, Gulnura verfasserin aut Dust storms in Kazakhstan: Frequency and division 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. Dust storms (dpeaa)DE-He213 soil texture (dpeaa)DE-He213 deserts (dpeaa)DE-He213 Kazakhstan (dpeaa)DE-He213 Central Asia (dpeaa)DE-He213 Abuduwaili, Jilili aut Kaldybayev, Azamat aut Semenov, Oleg aut Dedova, Tatiana aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 85(2015), 3 vom: März, Seite 348-358 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:85 year:2015 number:3 month:03 pages:348-358 https://dx.doi.org/10.1007/s12594-015-0224-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2015 3 03 348-358
allfieldsGer	10.1007/s12594-015-0224-5 doi (DE-627)SPR026211505 (SPR)s12594-015-0224-5-e DE-627 ger DE-627 rakwb eng Issanova, Gulnura verfasserin aut Dust storms in Kazakhstan: Frequency and division 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. Dust storms (dpeaa)DE-He213 soil texture (dpeaa)DE-He213 deserts (dpeaa)DE-He213 Kazakhstan (dpeaa)DE-He213 Central Asia (dpeaa)DE-He213 Abuduwaili, Jilili aut Kaldybayev, Azamat aut Semenov, Oleg aut Dedova, Tatiana aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 85(2015), 3 vom: März, Seite 348-358 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:85 year:2015 number:3 month:03 pages:348-358 https://dx.doi.org/10.1007/s12594-015-0224-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2015 3 03 348-358
allfieldsSound	10.1007/s12594-015-0224-5 doi (DE-627)SPR026211505 (SPR)s12594-015-0224-5-e DE-627 ger DE-627 rakwb eng Issanova, Gulnura verfasserin aut Dust storms in Kazakhstan: Frequency and division 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Geological Society of India 2015 Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. Dust storms (dpeaa)DE-He213 soil texture (dpeaa)DE-He213 deserts (dpeaa)DE-He213 Kazakhstan (dpeaa)DE-He213 Central Asia (dpeaa)DE-He213 Abuduwaili, Jilili aut Kaldybayev, Azamat aut Semenov, Oleg aut Dedova, Tatiana aut Enthalten in Journal of the Geological Society of India New Delhi : Springer India, 1959 85(2015), 3 vom: März, Seite 348-358 (DE-627)60666078X (DE-600)2508930-4 0974-6889 nnns volume:85 year:2015 number:3 month:03 pages:348-358 https://dx.doi.org/10.1007/s12594-015-0224-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 85 2015 3 03 348-358
language	English
source	Enthalten in Journal of the Geological Society of India 85(2015), 3 vom: März, Seite 348-358 volume:85 year:2015 number:3 month:03 pages:348-358
sourceStr	Enthalten in Journal of the Geological Society of India 85(2015), 3 vom: März, Seite 348-358 volume:85 year:2015 number:3 month:03 pages:348-358
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Dust storms soil texture deserts Kazakhstan Central Asia
isfreeaccess_bool	false
container_title	Journal of the Geological Society of India
authorswithroles_txt_mv	Issanova, Gulnura @@aut@@ Abuduwaili, Jilili @@aut@@ Kaldybayev, Azamat @@aut@@ Semenov, Oleg @@aut@@ Dedova, Tatiana @@aut@@
publishDateDaySort_date	2015-03-01T00:00:00Z
hierarchy_top_id	60666078X
id	SPR026211505
language_de	englisch
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author	Issanova, Gulnura
spellingShingle	Issanova, Gulnura misc Dust storms misc soil texture misc deserts misc Kazakhstan misc Central Asia Dust storms in Kazakhstan: Frequency and division
authorStr	Issanova, Gulnura
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topic_title	Dust storms in Kazakhstan: Frequency and division Dust storms (dpeaa)DE-He213 soil texture (dpeaa)DE-He213 deserts (dpeaa)DE-He213 Kazakhstan (dpeaa)DE-He213 Central Asia (dpeaa)DE-He213
topic	misc Dust storms misc soil texture misc deserts misc Kazakhstan misc Central Asia
topic_unstemmed	misc Dust storms misc soil texture misc deserts misc Kazakhstan misc Central Asia
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title	Dust storms in Kazakhstan: Frequency and division
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title_full	Dust storms in Kazakhstan: Frequency and division
author_sort	Issanova, Gulnura
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author_browse	Issanova, Gulnura Abuduwaili, Jilili Kaldybayev, Azamat Semenov, Oleg Dedova, Tatiana
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author-letter	Issanova, Gulnura
doi_str_mv	10.1007/s12594-015-0224-5
title_sort	dust storms in kazakhstan: frequency and division
title_auth	Dust storms in Kazakhstan: Frequency and division
abstract	Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. © Geological Society of India 2015
abstractGer	Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. © Geological Society of India 2015
abstract_unstemmed	Abstract Dust/sand storm is a common phenomenon in arid and semi-arid regions of Kazakhstan, especially in its southern parts, where areas are covered by a great variety of deserts and are a powerful source of mineral and salt aerosols. We considered the long-term meteorological data and satellite images on dust storms recurrence and their regional division in Kazakhstan. On the basis of generalization and analyses of the numerous cartographic materials, meteorological observations and satellite images, we identified seats of the powerful sources of dust/sand/salt storms. We found areas in Kazakhstan with the highest frequency of dust storms. These are Pre-Aral Karakum and Aralkum deserts; Kyzylkum and Moiynkum deserts; Ryn sands (northern Caspian plain); and southern Pre-Balkhash deserts. The most active source of dust storms is located in sandy deserts or in areas, which have suffered from human activity. Dust storms have a great negative impact on soil conditions and they are particularly dangerous for the environment. © Geological Society of India 2015
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title_short	Dust storms in Kazakhstan: Frequency and division
url	https://dx.doi.org/10.1007/s12594-015-0224-5
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author2	Abuduwaili, Jilili Kaldybayev, Azamat Semenov, Oleg Dedova, Tatiana
author2Str	Abuduwaili, Jilili Kaldybayev, Azamat Semenov, Oleg Dedova, Tatiana
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doi_str	10.1007/s12594-015-0224-5
up_date	2024-07-03T19:32:46.389Z
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