Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements
This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Easter...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Taylor Shingler [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2016 |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: Journal of geophysical research / D - Washington, DC : Union, 1984, 121(2016), 22 |
|---|---|
| Übergeordnetes Werk: |
volume:121 ; year:2016 ; number:22 |
| Links: |
|---|
| DOI / URN: |
10.1002/2016JD025471 |
|---|
| Katalog-ID: |
OLC1988774624 |
|---|
| LEADER | 01000caa a2200265 4500 | ||
|---|---|---|---|
| 001 | OLC1988774624 | ||
| 003 | DE-627 | ||
| 005 | 20230715023034.0 | ||
| 007 | tu | ||
| 008 | 170207s2016 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1002/2016JD025471 |2 doi | |
| 028 | 5 | 2 | |a PQ20170206 |
| 035 | |a (DE-627)OLC1988774624 | ||
| 035 | |a (DE-599)GBVOLC1988774624 | ||
| 035 | |a (PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0 | ||
| 035 | |a (KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q DNB |
| 100 | 0 | |a Taylor Shingler |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements |
| 264 | 1 | |c 2016 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 520 | |a This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 | ||
| 650 | 4 | |a Studies | |
| 650 | 4 | |a Growth factors | |
| 700 | 0 | |a Armin Sorooshian |4 oth | |
| 700 | 0 | |a Amber Ortega |4 oth | |
| 700 | 0 | |a Ewan Crosbie |4 oth | |
| 700 | 0 | |a Anna Wonaschutz |4 oth | |
| 700 | 0 | |a Anne E Perring |4 oth | |
| 700 | 0 | |a Andreas Beyersdorf |4 oth | |
| 700 | 0 | |a Luke Ziemba |4 oth | |
| 700 | 0 | |a Jose L Jimenez |4 oth | |
| 700 | 0 | |a Pedro Campuzano-Jost |4 oth | |
| 700 | 0 | |a Tomas Mikoviny |4 oth | |
| 700 | 0 | |a Armin Wisthaler |4 oth | |
| 700 | 0 | |a Lynn M Russell |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |t Journal of geophysical research / D |d Washington, DC : Union, 1984 |g 121(2016), 22 |w (DE-627)130444391 |w (DE-600)710256-2 |w (DE-576)015978818 |x 2169-897X |7 nnns |
| 773 | 1 | 8 | |g volume:121 |g year:2016 |g number:22 |
| 856 | 4 | 1 | |u http://dx.doi.org/10.1002/2016JD025471 |3 Volltext |
| 856 | 4 | 2 | |u http://search.proquest.com/docview/1847915132 |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-PHY | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a SSG-OPC-GEO | ||
| 912 | |a GBV_ILN_62 | ||
| 912 | |a GBV_ILN_154 | ||
| 951 | |a AR | ||
| 952 | |d 121 |j 2016 |e 22 | ||
| author_variant |
t s ts |
|---|---|
| matchkey_str |
article:2169897X:2016----::minosrainohgocpcrwhatrnfheo1aetdefosr |
| hierarchy_sort_str |
2016 |
| publishDate |
2016 |
| allfields |
10.1002/2016JD025471 doi PQ20170206 (DE-627)OLC1988774624 (DE-599)GBVOLC1988774624 (PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0 (KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh DE-627 ger DE-627 rakwb eng 550 DNB Taylor Shingler verfasserin aut Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 Studies Growth factors Armin Sorooshian oth Amber Ortega oth Ewan Crosbie oth Anna Wonaschutz oth Anne E Perring oth Andreas Beyersdorf oth Luke Ziemba oth Jose L Jimenez oth Pedro Campuzano-Jost oth Tomas Mikoviny oth Armin Wisthaler oth Lynn M Russell oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 121(2016), 22 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:121 year:2016 number:22 http://dx.doi.org/10.1002/2016JD025471 Volltext http://search.proquest.com/docview/1847915132 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 121 2016 22 |
| spelling |
10.1002/2016JD025471 doi PQ20170206 (DE-627)OLC1988774624 (DE-599)GBVOLC1988774624 (PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0 (KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh DE-627 ger DE-627 rakwb eng 550 DNB Taylor Shingler verfasserin aut Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 Studies Growth factors Armin Sorooshian oth Amber Ortega oth Ewan Crosbie oth Anna Wonaschutz oth Anne E Perring oth Andreas Beyersdorf oth Luke Ziemba oth Jose L Jimenez oth Pedro Campuzano-Jost oth Tomas Mikoviny oth Armin Wisthaler oth Lynn M Russell oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 121(2016), 22 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:121 year:2016 number:22 http://dx.doi.org/10.1002/2016JD025471 Volltext http://search.proquest.com/docview/1847915132 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 121 2016 22 |
| allfields_unstemmed |
10.1002/2016JD025471 doi PQ20170206 (DE-627)OLC1988774624 (DE-599)GBVOLC1988774624 (PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0 (KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh DE-627 ger DE-627 rakwb eng 550 DNB Taylor Shingler verfasserin aut Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 Studies Growth factors Armin Sorooshian oth Amber Ortega oth Ewan Crosbie oth Anna Wonaschutz oth Anne E Perring oth Andreas Beyersdorf oth Luke Ziemba oth Jose L Jimenez oth Pedro Campuzano-Jost oth Tomas Mikoviny oth Armin Wisthaler oth Lynn M Russell oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 121(2016), 22 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:121 year:2016 number:22 http://dx.doi.org/10.1002/2016JD025471 Volltext http://search.proquest.com/docview/1847915132 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 121 2016 22 |
| allfieldsGer |
10.1002/2016JD025471 doi PQ20170206 (DE-627)OLC1988774624 (DE-599)GBVOLC1988774624 (PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0 (KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh DE-627 ger DE-627 rakwb eng 550 DNB Taylor Shingler verfasserin aut Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 Studies Growth factors Armin Sorooshian oth Amber Ortega oth Ewan Crosbie oth Anna Wonaschutz oth Anne E Perring oth Andreas Beyersdorf oth Luke Ziemba oth Jose L Jimenez oth Pedro Campuzano-Jost oth Tomas Mikoviny oth Armin Wisthaler oth Lynn M Russell oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 121(2016), 22 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:121 year:2016 number:22 http://dx.doi.org/10.1002/2016JD025471 Volltext http://search.proquest.com/docview/1847915132 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 121 2016 22 |
| allfieldsSound |
10.1002/2016JD025471 doi PQ20170206 (DE-627)OLC1988774624 (DE-599)GBVOLC1988774624 (PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0 (KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh DE-627 ger DE-627 rakwb eng 550 DNB Taylor Shingler verfasserin aut Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 Studies Growth factors Armin Sorooshian oth Amber Ortega oth Ewan Crosbie oth Anna Wonaschutz oth Anne E Perring oth Andreas Beyersdorf oth Luke Ziemba oth Jose L Jimenez oth Pedro Campuzano-Jost oth Tomas Mikoviny oth Armin Wisthaler oth Lynn M Russell oth Enthalten in Journal of geophysical research / D Washington, DC : Union, 1984 121(2016), 22 (DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 2169-897X nnns volume:121 year:2016 number:22 http://dx.doi.org/10.1002/2016JD025471 Volltext http://search.proquest.com/docview/1847915132 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 AR 121 2016 22 |
| language |
English |
| source |
Enthalten in Journal of geophysical research / D 121(2016), 22 volume:121 year:2016 number:22 |
| sourceStr |
Enthalten in Journal of geophysical research / D 121(2016), 22 volume:121 year:2016 number:22 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Studies Growth factors |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Journal of geophysical research / D |
| authorswithroles_txt_mv |
Taylor Shingler @@aut@@ Armin Sorooshian @@oth@@ Amber Ortega @@oth@@ Ewan Crosbie @@oth@@ Anna Wonaschutz @@oth@@ Anne E Perring @@oth@@ Andreas Beyersdorf @@oth@@ Luke Ziemba @@oth@@ Jose L Jimenez @@oth@@ Pedro Campuzano-Jost @@oth@@ Tomas Mikoviny @@oth@@ Armin Wisthaler @@oth@@ Lynn M Russell @@oth@@ |
| publishDateDaySort_date |
2016-01-01T00:00:00Z |
| hierarchy_top_id |
130444391 |
| dewey-sort |
3550 |
| id |
OLC1988774624 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1988774624</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230715023034.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">170207s2016 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1002/2016JD025471</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20170206</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1988774624</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1988774624</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh</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">550</subfield><subfield code="q">DNB</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Taylor Shingler</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Studies</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Growth factors</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Armin Sorooshian</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Amber Ortega</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Ewan Crosbie</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Anna Wonaschutz</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Anne E Perring</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Andreas Beyersdorf</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Luke Ziemba</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jose L Jimenez</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Pedro Campuzano-Jost</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Tomas Mikoviny</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Armin Wisthaler</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Lynn M Russell</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of geophysical research / D</subfield><subfield code="d">Washington, DC : Union, 1984</subfield><subfield code="g">121(2016), 22</subfield><subfield code="w">(DE-627)130444391</subfield><subfield code="w">(DE-600)710256-2</subfield><subfield code="w">(DE-576)015978818</subfield><subfield code="x">2169-897X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:121</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:22</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1002/2016JD025471</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1847915132</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">121</subfield><subfield code="j">2016</subfield><subfield code="e">22</subfield></datafield></record></collection>
|
| author |
Taylor Shingler |
| spellingShingle |
Taylor Shingler ddc 550 misc Studies misc Growth factors Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements |
| authorStr |
Taylor Shingler |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)130444391 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
2169-897X |
| topic_title |
550 DNB Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements Studies Growth factors |
| topic |
ddc 550 misc Studies misc Growth factors |
| topic_unstemmed |
ddc 550 misc Studies misc Growth factors |
| topic_browse |
ddc 550 misc Studies misc Growth factors |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| author2_variant |
a s as a o ao e c ec a w aw a e p aep a b ab l z lz j l j jlj p c j pcj t m tm a w aw l m r lmr |
| hierarchy_parent_title |
Journal of geophysical research / D |
| hierarchy_parent_id |
130444391 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Journal of geophysical research / D |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)130444391 (DE-600)710256-2 (DE-576)015978818 |
| title |
Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements |
| ctrlnum |
(DE-627)OLC1988774624 (DE-599)GBVOLC1988774624 (PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0 (KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh |
| title_full |
Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements |
| author_sort |
Taylor Shingler |
| journal |
Journal of geophysical research / D |
| journalStr |
Journal of geophysical research / D |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2016 |
| contenttype_str_mv |
txt |
| author_browse |
Taylor Shingler |
| container_volume |
121 |
| class |
550 DNB |
| format_se |
Aufsätze |
| author-letter |
Taylor Shingler |
| doi_str_mv |
10.1002/2016JD025471 |
| dewey-full |
550 |
| title_sort |
ambient observations of hygroscopic growth factor and f(rh) below 1: case studies from surface and airborne measurements |
| title_auth |
Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements |
| abstract |
This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 |
| abstractGer |
This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 |
| abstract_unstemmed |
This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 |
| container_issue |
22 |
| title_short |
Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements |
| url |
http://dx.doi.org/10.1002/2016JD025471 http://search.proquest.com/docview/1847915132 |
| remote_bool |
false |
| author2 |
Armin Sorooshian Amber Ortega Ewan Crosbie Anna Wonaschutz Anne E Perring Andreas Beyersdorf Luke Ziemba Jose L Jimenez Pedro Campuzano-Jost Tomas Mikoviny Armin Wisthaler Lynn M Russell |
| author2Str |
Armin Sorooshian Amber Ortega Ewan Crosbie Anna Wonaschutz Anne E Perring Andreas Beyersdorf Luke Ziemba Jose L Jimenez Pedro Campuzano-Jost Tomas Mikoviny Armin Wisthaler Lynn M Russell |
| ppnlink |
130444391 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth oth oth oth oth oth oth oth oth oth |
| doi_str |
10.1002/2016JD025471 |
| up_date |
2024-07-03T19:11:23.488Z |
| _version_ |
1803586249415458816 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC1988774624</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230715023034.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">170207s2016 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1002/2016JD025471</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20170206</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC1988774624</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC1988774624</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p1170-9a9d0d141a68778122b1dcb1a202ece2a987782129310c939814200507efd47f0</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0137985220160000121002200000ambientobservationsofhygroscopicgrowthfactorandfrh</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">550</subfield><subfield code="q">DNB</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Taylor Shingler</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Ambient observations of hygroscopic growth factor and f(RH) below 1: Case studies from surface and airborne measurements</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">This study reports a detailed set of ambient observations of optical/physical shrinking of particles from exposure to water vapor with consistency across different instruments and regions. Data have been utilized from (i) a shipboard humidified tandem differential mobility analyzer during the Eastern Pacific Emitted Aerosol Cloud Experiment in 2011, (ii) multiple instruments on the NASA DC-8 research aircraft during the Studies of Emissions, Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys in 2013, and (iii) the Differential Aerosol Sizing and Hygroscopicity Spectrometer Probe during ambient measurements in Tucson, Arizona, during summer 2014 and winter 2015. Hygroscopic growth factor (ratio of humidified-to-dry diameter, GF=Dp,wet/Dp,dry) and f(RH) (ratio of humidified-to-dry scattering coefficients) values below 1 were observed across the range of relative humidity (RH) investigated (75-95%). A commonality of observations of GF and f(RH) below 1 in these experiments was the presence of particles enriched with carbonaceous matter, especially from biomass burning. Evidence of externally mixed aerosol, and thus multiple GFs with at least one GF<1, was observed concurrently with f(RH)<1 during smoke periods. Possible mechanisms responsible for observed shrinkage are discussed and include particle restructuring, volatilization effects, and refractive index modifications due to aqueous processing resulting in optical size modification. To further investigate ambient observations of GFs and f(RH) values less than 1, it is recommended to add an optional prehumidification bypass module to hygroscopicity instruments, to preemptively collapse particles prior to controlled RH measurements. Key Points Observations are reported for growth factor (GF) and f(RH) values below 1 in multiple regions using three instruments GF and f(RH) values less than 1 are observed in biomass burning plumes, organic-rich particles, and wintertime in an urban area f(RH) increases as a function of effective particle density with the majority of values below 1 coincident with density <1.2gcm-3</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Studies</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Growth factors</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Armin Sorooshian</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Amber Ortega</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Ewan Crosbie</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Anna Wonaschutz</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Anne E Perring</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Andreas Beyersdorf</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Luke Ziemba</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Jose L Jimenez</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Pedro Campuzano-Jost</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Tomas Mikoviny</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Armin Wisthaler</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Lynn M Russell</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of geophysical research / D</subfield><subfield code="d">Washington, DC : Union, 1984</subfield><subfield code="g">121(2016), 22</subfield><subfield code="w">(DE-627)130444391</subfield><subfield code="w">(DE-600)710256-2</subfield><subfield code="w">(DE-576)015978818</subfield><subfield code="x">2169-897X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:121</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:22</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.1002/2016JD025471</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1847915132</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">121</subfield><subfield code="j">2016</subfield><subfield code="e">22</subfield></datafield></record></collection>
|
| score |
7.40226 |