The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$
Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which ma...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhang, Xiaobing [verfasserIn] Li, Dongfeng [verfasserIn] Bo, Tianli [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2018 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Granular matter - Berlin : Springer, 1998, 20(2018), 3 vom: 04. Mai |
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| Übergeordnetes Werk: |
volume:20 ; year:2018 ; number:3 ; day:04 ; month:05 |
| Links: |
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| DOI / URN: |
10.1007/s10035-018-0801-6 |
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| Katalog-ID: |
SPR008144591 |
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| 100 | 1 | |a Zhang, Xiaobing |e verfasserin |4 aut | |
| 245 | 1 | 4 | |a The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ |
| 264 | 1 | |c 2018 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
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| 520 | |a Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. | ||
| 650 | 4 | |a Dust storm |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Vertical electric field |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Charge to mass ratio |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Stratification |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Ambient temperature |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Li, Dongfeng |e verfasserin |4 aut | |
| 700 | 1 | |a Bo, Tianli |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Granular matter |d Berlin : Springer, 1998 |g 20(2018), 3 vom: 04. Mai |w (DE-627)300183771 |w (DE-600)1481431-6 |x 1434-7636 |7 nnns |
| 773 | 1 | 8 | |g volume:20 |g year:2018 |g number:3 |g day:04 |g month:05 |
| 856 | 4 | 0 | |u https://dx.doi.org/10.1007/s10035-018-0801-6 |z lizenzpflichtig |3 Volltext |
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10.1007/s10035-018-0801-6 doi (DE-627)SPR008144591 (SPR)s10035-018-0801-6-e DE-627 ger DE-627 rakwb eng 500 ASE 38.58 bkl 33.61 bkl 50.35 bkl Zhang, Xiaobing verfasserin aut The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. Dust storm (dpeaa)DE-He213 Vertical electric field (dpeaa)DE-He213 Charge to mass ratio (dpeaa)DE-He213 Stratification (dpeaa)DE-He213 Ambient temperature (dpeaa)DE-He213 Li, Dongfeng verfasserin aut Bo, Tianli verfasserin aut Enthalten in Granular matter Berlin : Springer, 1998 20(2018), 3 vom: 04. Mai (DE-627)300183771 (DE-600)1481431-6 1434-7636 nnns volume:20 year:2018 number:3 day:04 month:05 https://dx.doi.org/10.1007/s10035-018-0801-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE 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_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_152 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_267 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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 38.58 ASE 33.61 ASE 50.35 ASE AR 20 2018 3 04 05 |
| spelling |
10.1007/s10035-018-0801-6 doi (DE-627)SPR008144591 (SPR)s10035-018-0801-6-e DE-627 ger DE-627 rakwb eng 500 ASE 38.58 bkl 33.61 bkl 50.35 bkl Zhang, Xiaobing verfasserin aut The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. Dust storm (dpeaa)DE-He213 Vertical electric field (dpeaa)DE-He213 Charge to mass ratio (dpeaa)DE-He213 Stratification (dpeaa)DE-He213 Ambient temperature (dpeaa)DE-He213 Li, Dongfeng verfasserin aut Bo, Tianli verfasserin aut Enthalten in Granular matter Berlin : Springer, 1998 20(2018), 3 vom: 04. Mai (DE-627)300183771 (DE-600)1481431-6 1434-7636 nnns volume:20 year:2018 number:3 day:04 month:05 https://dx.doi.org/10.1007/s10035-018-0801-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE 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_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_152 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_267 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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 38.58 ASE 33.61 ASE 50.35 ASE AR 20 2018 3 04 05 |
| allfields_unstemmed |
10.1007/s10035-018-0801-6 doi (DE-627)SPR008144591 (SPR)s10035-018-0801-6-e DE-627 ger DE-627 rakwb eng 500 ASE 38.58 bkl 33.61 bkl 50.35 bkl Zhang, Xiaobing verfasserin aut The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. Dust storm (dpeaa)DE-He213 Vertical electric field (dpeaa)DE-He213 Charge to mass ratio (dpeaa)DE-He213 Stratification (dpeaa)DE-He213 Ambient temperature (dpeaa)DE-He213 Li, Dongfeng verfasserin aut Bo, Tianli verfasserin aut Enthalten in Granular matter Berlin : Springer, 1998 20(2018), 3 vom: 04. Mai (DE-627)300183771 (DE-600)1481431-6 1434-7636 nnns volume:20 year:2018 number:3 day:04 month:05 https://dx.doi.org/10.1007/s10035-018-0801-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE 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_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_152 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_267 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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 38.58 ASE 33.61 ASE 50.35 ASE AR 20 2018 3 04 05 |
| allfieldsGer |
10.1007/s10035-018-0801-6 doi (DE-627)SPR008144591 (SPR)s10035-018-0801-6-e DE-627 ger DE-627 rakwb eng 500 ASE 38.58 bkl 33.61 bkl 50.35 bkl Zhang, Xiaobing verfasserin aut The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. Dust storm (dpeaa)DE-He213 Vertical electric field (dpeaa)DE-He213 Charge to mass ratio (dpeaa)DE-He213 Stratification (dpeaa)DE-He213 Ambient temperature (dpeaa)DE-He213 Li, Dongfeng verfasserin aut Bo, Tianli verfasserin aut Enthalten in Granular matter Berlin : Springer, 1998 20(2018), 3 vom: 04. Mai (DE-627)300183771 (DE-600)1481431-6 1434-7636 nnns volume:20 year:2018 number:3 day:04 month:05 https://dx.doi.org/10.1007/s10035-018-0801-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE 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_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_152 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_267 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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 38.58 ASE 33.61 ASE 50.35 ASE AR 20 2018 3 04 05 |
| allfieldsSound |
10.1007/s10035-018-0801-6 doi (DE-627)SPR008144591 (SPR)s10035-018-0801-6-e DE-627 ger DE-627 rakwb eng 500 ASE 38.58 bkl 33.61 bkl 50.35 bkl Zhang, Xiaobing verfasserin aut The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. Dust storm (dpeaa)DE-He213 Vertical electric field (dpeaa)DE-He213 Charge to mass ratio (dpeaa)DE-He213 Stratification (dpeaa)DE-He213 Ambient temperature (dpeaa)DE-He213 Li, Dongfeng verfasserin aut Bo, Tianli verfasserin aut Enthalten in Granular matter Berlin : Springer, 1998 20(2018), 3 vom: 04. Mai (DE-627)300183771 (DE-600)1481431-6 1434-7636 nnns volume:20 year:2018 number:3 day:04 month:05 https://dx.doi.org/10.1007/s10035-018-0801-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE 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_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_152 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_267 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_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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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 38.58 ASE 33.61 ASE 50.35 ASE AR 20 2018 3 04 05 |
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English |
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Enthalten in Granular matter 20(2018), 3 vom: 04. Mai volume:20 year:2018 number:3 day:04 month:05 |
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findex.gbv.de |
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Dust storm Vertical electric field Charge to mass ratio Stratification Ambient temperature |
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Zhang, Xiaobing @@aut@@ Li, Dongfeng @@aut@@ Bo, Tianli @@aut@@ |
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2018-05-04T00:00:00Z |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR008144591</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110201053.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s2018 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10035-018-0801-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR008144591</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s10035-018-0801-6-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">500</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.58</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">33.61</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">50.35</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhang, Xiaobing</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="4"><subfield code="a">The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2018</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Dust storm</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Vertical electric field</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Charge to mass ratio</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stratification</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ambient temperature</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Dongfeng</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bo, Tianli</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Granular matter</subfield><subfield code="d">Berlin : Springer, 1998</subfield><subfield code="g">20(2018), 3 vom: 04. 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|
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Zhang, Xiaobing |
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Zhang, Xiaobing ddc 500 bkl 38.58 bkl 33.61 bkl 50.35 misc Dust storm misc Vertical electric field misc Charge to mass ratio misc Stratification misc Ambient temperature The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ |
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500 ASE 38.58 bkl 33.61 bkl 50.35 bkl The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ Dust storm (dpeaa)DE-He213 Vertical electric field (dpeaa)DE-He213 Charge to mass ratio (dpeaa)DE-He213 Stratification (dpeaa)DE-He213 Ambient temperature (dpeaa)DE-He213 |
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ddc 500 bkl 38.58 bkl 33.61 bkl 50.35 misc Dust storm misc Vertical electric field misc Charge to mass ratio misc Stratification misc Ambient temperature |
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ddc 500 bkl 38.58 bkl 33.61 bkl 50.35 misc Dust storm misc Vertical electric field misc Charge to mass ratio misc Stratification misc Ambient temperature |
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The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ |
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The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ |
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Zhang, Xiaobing Li, Dongfeng Bo, Tianli |
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variation of the vertical electric field (%${{\varvec{e}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{e}}}_{\mathrm{z}}%$ |
| title_auth |
The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ |
| abstract |
Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. |
| abstractGer |
Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. |
| abstract_unstemmed |
Abstract Field observations were carried out in Qingtu Lake observation array on the vertical electric field %$(E_{z})%$, where the average spatial resolution can reach 1 m. Our results show that %$E_{z}%$ can be approximately divided into six layers according to the direction of %$E_{z}%$, which may be caused by the stratification of the polarity of the charged dust particles, and this phenomenon is prevalent in development stage, stable stage and decay stage of dust storms. It demonstrates that the spatial distributions of %$E_{z}%$ and charge to mass ratio of dust particles in different stages have the similar pattern. Moreover, the intensities of %$E_{z}%$ in the development and decay stages are less than that in the stable stage, which may be caused by the difference of dust concentration. Our results show that the ambient temperature will also affect the vertical electric field besides the dust concentration during dust storms, i.e., %$E_{z}%$ increases with the ambient temperature. |
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| container_issue |
3 |
| title_short |
The variation of the vertical electric field (%${{\varvec{E}}}_{\mathrm{z}}%$) with height during dust storms and the effects of environmental variables on %${{\varvec{E}}}_{\mathrm{z}}%$ |
| url |
https://dx.doi.org/10.1007/s10035-018-0801-6 |
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true |
| author2 |
Li, Dongfeng Bo, Tianli |
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Li, Dongfeng Bo, Tianli |
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| doi_str |
10.1007/s10035-018-0801-6 |
| up_date |
2024-07-03T17:35:27.892Z |
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1803580214236676096 |
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|
| score |
7.40125 |