UV radiation in the southern seas in early spring 1993
Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some...
Ausführliche Beschreibung
Autor*in: |
Wendler, G. [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
1996 |
---|
Schlagwörter: |
---|
Systematik: |
|
---|
Anmerkung: |
© Springer-Verlag 1996 |
---|
Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer-Verlag, 1986, 53(1996), 4 vom: Dez., Seite 221-230 |
---|---|
Übergeordnetes Werk: |
volume:53 ; year:1996 ; number:4 ; month:12 ; pages:221-230 |
Links: |
---|
DOI / URN: |
10.1007/BF00871738 |
---|
Katalog-ID: |
OLC2048433979 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2048433979 | ||
003 | DE-627 | ||
005 | 20230502135603.0 | ||
007 | tu | ||
008 | 200820s1996 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/BF00871738 |2 doi | |
035 | |a (DE-627)OLC2048433979 | ||
035 | |a (DE-He213)BF00871738-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 14 |2 ssgn | ||
084 | |a RA 1000 |q VZ |2 rvk | ||
100 | 1 | |a Wendler, G. |e verfasserin |4 aut | |
245 | 1 | 0 | |a UV radiation in the southern seas in early spring 1993 |
264 | 1 | |c 1996 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © Springer-Verlag 1996 | ||
520 | |a Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. | ||
650 | 4 | |a Ozone | |
650 | 4 | |a Ozone Concentration | |
650 | 4 | |a Radiation Level | |
650 | 4 | |a Global Radiation | |
650 | 4 | |a Ozone Level | |
700 | 1 | |a Quakenbush, T. |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Theoretical and applied climatology |d Springer-Verlag, 1986 |g 53(1996), 4 vom: Dez., Seite 221-230 |w (DE-627)129958808 |w (DE-600)405799-5 |w (DE-576)01552857X |x 0177-798X |7 nnns |
773 | 1 | 8 | |g volume:53 |g year:1996 |g number:4 |g month:12 |g pages:221-230 |
856 | 4 | 1 | |u https://doi.org/10.1007/BF00871738 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
912 | |a GBV_ILN_11 | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_31 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_130 | ||
912 | |a GBV_ILN_601 | ||
912 | |a GBV_ILN_2001 | ||
912 | |a GBV_ILN_2006 | ||
912 | |a GBV_ILN_2010 | ||
912 | |a GBV_ILN_2014 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4029 | ||
912 | |a GBV_ILN_4037 | ||
912 | |a GBV_ILN_4103 | ||
912 | |a GBV_ILN_4305 | ||
912 | |a GBV_ILN_4306 | ||
912 | |a GBV_ILN_4311 | ||
912 | |a GBV_ILN_4313 | ||
912 | |a GBV_ILN_4325 | ||
912 | |a GBV_ILN_4330 | ||
936 | r | v | |a RA 1000 |
951 | |a AR | ||
952 | |d 53 |j 1996 |e 4 |c 12 |h 221-230 |
author_variant |
g w gw t q tq |
---|---|
matchkey_str |
article:0177798X:1996----::vaitoiteotenesna |
hierarchy_sort_str |
1996 |
publishDate |
1996 |
allfields |
10.1007/BF00871738 doi (DE-627)OLC2048433979 (DE-He213)BF00871738-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wendler, G. verfasserin aut UV radiation in the southern seas in early spring 1993 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. Ozone Ozone Concentration Radiation Level Global Radiation Ozone Level Quakenbush, T. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 53(1996), 4 vom: Dez., Seite 221-230 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:53 year:1996 number:4 month:12 pages:221-230 https://doi.org/10.1007/BF00871738 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4037 GBV_ILN_4103 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4325 GBV_ILN_4330 RA 1000 AR 53 1996 4 12 221-230 |
spelling |
10.1007/BF00871738 doi (DE-627)OLC2048433979 (DE-He213)BF00871738-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wendler, G. verfasserin aut UV radiation in the southern seas in early spring 1993 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. Ozone Ozone Concentration Radiation Level Global Radiation Ozone Level Quakenbush, T. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 53(1996), 4 vom: Dez., Seite 221-230 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:53 year:1996 number:4 month:12 pages:221-230 https://doi.org/10.1007/BF00871738 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4037 GBV_ILN_4103 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4325 GBV_ILN_4330 RA 1000 AR 53 1996 4 12 221-230 |
allfields_unstemmed |
10.1007/BF00871738 doi (DE-627)OLC2048433979 (DE-He213)BF00871738-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wendler, G. verfasserin aut UV radiation in the southern seas in early spring 1993 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. Ozone Ozone Concentration Radiation Level Global Radiation Ozone Level Quakenbush, T. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 53(1996), 4 vom: Dez., Seite 221-230 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:53 year:1996 number:4 month:12 pages:221-230 https://doi.org/10.1007/BF00871738 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4037 GBV_ILN_4103 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4325 GBV_ILN_4330 RA 1000 AR 53 1996 4 12 221-230 |
allfieldsGer |
10.1007/BF00871738 doi (DE-627)OLC2048433979 (DE-He213)BF00871738-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wendler, G. verfasserin aut UV radiation in the southern seas in early spring 1993 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. Ozone Ozone Concentration Radiation Level Global Radiation Ozone Level Quakenbush, T. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 53(1996), 4 vom: Dez., Seite 221-230 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:53 year:1996 number:4 month:12 pages:221-230 https://doi.org/10.1007/BF00871738 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4037 GBV_ILN_4103 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4325 GBV_ILN_4330 RA 1000 AR 53 1996 4 12 221-230 |
allfieldsSound |
10.1007/BF00871738 doi (DE-627)OLC2048433979 (DE-He213)BF00871738-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Wendler, G. verfasserin aut UV radiation in the southern seas in early spring 1993 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. Ozone Ozone Concentration Radiation Level Global Radiation Ozone Level Quakenbush, T. aut Enthalten in Theoretical and applied climatology Springer-Verlag, 1986 53(1996), 4 vom: Dez., Seite 221-230 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:53 year:1996 number:4 month:12 pages:221-230 https://doi.org/10.1007/BF00871738 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4037 GBV_ILN_4103 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4325 GBV_ILN_4330 RA 1000 AR 53 1996 4 12 221-230 |
language |
English |
source |
Enthalten in Theoretical and applied climatology 53(1996), 4 vom: Dez., Seite 221-230 volume:53 year:1996 number:4 month:12 pages:221-230 |
sourceStr |
Enthalten in Theoretical and applied climatology 53(1996), 4 vom: Dez., Seite 221-230 volume:53 year:1996 number:4 month:12 pages:221-230 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Ozone Ozone Concentration Radiation Level Global Radiation Ozone Level |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Theoretical and applied climatology |
authorswithroles_txt_mv |
Wendler, G. @@aut@@ Quakenbush, T. @@aut@@ |
publishDateDaySort_date |
1996-12-01T00:00:00Z |
hierarchy_top_id |
129958808 |
dewey-sort |
3550 |
id |
OLC2048433979 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2048433979</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502135603.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s1996 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF00871738</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2048433979</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF00871738-p</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">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Wendler, G.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">UV radiation in the southern seas in early spring 1993</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1996</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="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 1996</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone Concentration</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Radiation Level</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Global Radiation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone Level</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Quakenbush, T.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Theoretical and applied climatology</subfield><subfield code="d">Springer-Verlag, 1986</subfield><subfield code="g">53(1996), 4 vom: Dez., Seite 221-230</subfield><subfield code="w">(DE-627)129958808</subfield><subfield code="w">(DE-600)405799-5</subfield><subfield code="w">(DE-576)01552857X</subfield><subfield code="x">0177-798X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:53</subfield><subfield code="g">year:1996</subfield><subfield code="g">number:4</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:221-230</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF00871738</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_130</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4029</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4103</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4311</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4330</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">53</subfield><subfield code="j">1996</subfield><subfield code="e">4</subfield><subfield code="c">12</subfield><subfield code="h">221-230</subfield></datafield></record></collection>
|
author |
Wendler, G. |
spellingShingle |
Wendler, G. ddc 550 ssgn 14 rvk RA 1000 misc Ozone misc Ozone Concentration misc Radiation Level misc Global Radiation misc Ozone Level UV radiation in the southern seas in early spring 1993 |
authorStr |
Wendler, G. |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)129958808 |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0177-798X |
topic_title |
550 VZ 14 ssgn RA 1000 VZ rvk UV radiation in the southern seas in early spring 1993 Ozone Ozone Concentration Radiation Level Global Radiation Ozone Level |
topic |
ddc 550 ssgn 14 rvk RA 1000 misc Ozone misc Ozone Concentration misc Radiation Level misc Global Radiation misc Ozone Level |
topic_unstemmed |
ddc 550 ssgn 14 rvk RA 1000 misc Ozone misc Ozone Concentration misc Radiation Level misc Global Radiation misc Ozone Level |
topic_browse |
ddc 550 ssgn 14 rvk RA 1000 misc Ozone misc Ozone Concentration misc Radiation Level misc Global Radiation misc Ozone Level |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Theoretical and applied climatology |
hierarchy_parent_id |
129958808 |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Theoretical and applied climatology |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X |
title |
UV radiation in the southern seas in early spring 1993 |
ctrlnum |
(DE-627)OLC2048433979 (DE-He213)BF00871738-p |
title_full |
UV radiation in the southern seas in early spring 1993 |
author_sort |
Wendler, G. |
journal |
Theoretical and applied climatology |
journalStr |
Theoretical and applied climatology |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
1996 |
contenttype_str_mv |
txt |
container_start_page |
221 |
author_browse |
Wendler, G. Quakenbush, T. |
container_volume |
53 |
class |
550 VZ 14 ssgn RA 1000 VZ rvk |
format_se |
Aufsätze |
author-letter |
Wendler, G. |
doi_str_mv |
10.1007/BF00871738 |
dewey-full |
550 |
title_sort |
uv radiation in the southern seas in early spring 1993 |
title_auth |
UV radiation in the southern seas in early spring 1993 |
abstract |
Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. © Springer-Verlag 1996 |
abstractGer |
Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. © Springer-Verlag 1996 |
abstract_unstemmed |
Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected. © Springer-Verlag 1996 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2001 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4037 GBV_ILN_4103 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4325 GBV_ILN_4330 |
container_issue |
4 |
title_short |
UV radiation in the southern seas in early spring 1993 |
url |
https://doi.org/10.1007/BF00871738 |
remote_bool |
false |
author2 |
Quakenbush, T. |
author2Str |
Quakenbush, T. |
ppnlink |
129958808 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/BF00871738 |
up_date |
2024-07-03T18:42:31.436Z |
_version_ |
1803584433228349440 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2048433979</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502135603.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s1996 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/BF00871738</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2048433979</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)BF00871738-p</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">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Wendler, G.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">UV radiation in the southern seas in early spring 1993</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1996</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="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag 1996</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Summary Radiation measurements were carried out during a research cruise of theN. Palmer in August and September 1993, from the tip of South America to Antarctica. As the measurements were carried out on a moving platform their validity had to be confirmed. This was undertaken for hourly data. Some of the main results are as follows:The radiation levels changed substantially during the cruise, as both latitude and season changed. Daily values of global, UV-A and UV-B radiation are presented.The mean value of the clearness indexKt (total transmissivity) was found to be 0.44. This is rather a low value, however, the cloudiness was high (mean value 78%). The clearness index increased with decreasing cloudiness from 0.41 for overcast conditions to 0.62 for clear sky conditions. Individual daily values varied even more, but always ranged between 0.2 and 0.8.The UV-A and UV-B radiation levels were related to the global radiation. However, correlation coefficients improved substantially when the analysis was carried out for different cloudiness classes. Clouds produced the largest reduction in global radiation and reduced UV-A and then UV-B to a lesser extent.As can be deduced from the previous bullet point therelative intensity of the UV radiation increased with cloudiness. This was more pronounced for UV-B than for UV-A.Ozone concentrations during the trip varied between 160 to 290 DU (Dobson Units). We passed under the “Antarctic ozone hole” several times during the cruise.UV-B radiation levels were affected by ozone levels and cloudiness. A 3-dimensional presentation is presented for UV-B versus ozone and cloudiness.UV-B radiation levels were, on average, more than double the average whilst under the “Antarctic ozone hole”, whereas UV-A radiation levels were hardly affected.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone Concentration</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Radiation Level</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Global Radiation</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ozone Level</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Quakenbush, T.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Theoretical and applied climatology</subfield><subfield code="d">Springer-Verlag, 1986</subfield><subfield code="g">53(1996), 4 vom: Dez., Seite 221-230</subfield><subfield code="w">(DE-627)129958808</subfield><subfield code="w">(DE-600)405799-5</subfield><subfield code="w">(DE-576)01552857X</subfield><subfield code="x">0177-798X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:53</subfield><subfield code="g">year:1996</subfield><subfield code="g">number:4</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:221-230</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/BF00871738</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_130</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4029</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4103</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4311</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4330</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">53</subfield><subfield code="j">1996</subfield><subfield code="e">4</subfield><subfield code="c">12</subfield><subfield code="h">221-230</subfield></datafield></record></collection>
|
score |
7.4002237 |