A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission
Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry,...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1988 |
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| Umfang: |
7 |
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| Reproduktion: |
Springer Online Journal Archives 1860-2002 |
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| Übergeordnetes Werk: |
in: Microchimica acta - 1937, 95(1988) vom: Jan./Juni, Seite 421-427 |
| Übergeordnetes Werk: |
volume:95 ; year:1988 ; month:01/06 ; pages:421-427 ; extent:7 |
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NLEJ207833176 |
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| 520 | |a Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). | ||
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| 700 | 1 | |a Revercomb, Henry E. |4 oth | |
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(DE-627)NLEJ207833176 DE-627 ger DE-627 rakwb eng A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission 1988 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). Springer Online Journal Archives 1860-2002 LaPorte, Daniel D. oth Carpenter, James D. oth Revercomb, Henry E. oth in Microchimica acta 1937 95(1988) vom: Jan./Juni, Seite 421-427 (DE-627)NLEJ188993894 (DE-600)1462152-6 1436-5073 nnns volume:95 year:1988 month:01/06 pages:421-427 extent:7 http://dx.doi.org/10.1007/BF01349801 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 95 1988 1/6 421-427 7 |
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(DE-627)NLEJ207833176 DE-627 ger DE-627 rakwb eng A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission 1988 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). Springer Online Journal Archives 1860-2002 LaPorte, Daniel D. oth Carpenter, James D. oth Revercomb, Henry E. oth in Microchimica acta 1937 95(1988) vom: Jan./Juni, Seite 421-427 (DE-627)NLEJ188993894 (DE-600)1462152-6 1436-5073 nnns volume:95 year:1988 month:01/06 pages:421-427 extent:7 http://dx.doi.org/10.1007/BF01349801 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 95 1988 1/6 421-427 7 |
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(DE-627)NLEJ207833176 DE-627 ger DE-627 rakwb eng A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission 1988 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). Springer Online Journal Archives 1860-2002 LaPorte, Daniel D. oth Carpenter, James D. oth Revercomb, Henry E. oth in Microchimica acta 1937 95(1988) vom: Jan./Juni, Seite 421-427 (DE-627)NLEJ188993894 (DE-600)1462152-6 1436-5073 nnns volume:95 year:1988 month:01/06 pages:421-427 extent:7 http://dx.doi.org/10.1007/BF01349801 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 95 1988 1/6 421-427 7 |
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(DE-627)NLEJ207833176 DE-627 ger DE-627 rakwb eng A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission 1988 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). Springer Online Journal Archives 1860-2002 LaPorte, Daniel D. oth Carpenter, James D. oth Revercomb, Henry E. oth in Microchimica acta 1937 95(1988) vom: Jan./Juni, Seite 421-427 (DE-627)NLEJ188993894 (DE-600)1462152-6 1436-5073 nnns volume:95 year:1988 month:01/06 pages:421-427 extent:7 http://dx.doi.org/10.1007/BF01349801 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 95 1988 1/6 421-427 7 |
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(DE-627)NLEJ207833176 DE-627 ger DE-627 rakwb eng A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission 1988 7 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). Springer Online Journal Archives 1860-2002 LaPorte, Daniel D. oth Carpenter, James D. oth Revercomb, Henry E. oth in Microchimica acta 1937 95(1988) vom: Jan./Juni, Seite 421-427 (DE-627)NLEJ188993894 (DE-600)1462152-6 1436-5073 nnns volume:95 year:1988 month:01/06 pages:421-427 extent:7 http://dx.doi.org/10.1007/BF01349801 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 95 1988 1/6 421-427 7 |
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a radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission |
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A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission |
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Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). |
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Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). |
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Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment). |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ207833176</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707000525.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">070528s1988 xx |||||o 00| ||eng c</controlfield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ207833176</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="245" ind1="1" ind2="0"><subfield code="a">A radiometrie fourier transform spectrometer for the measurement of downwelling atmospheric emission</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">1988</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">7</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Radiometrically accurate downwelling emission from the atmosphere has been measured using a ground-based ambient temperature Michelson interferometer with a liquid-helium-cooled SiAs detector. Measurements were made under a wide range of atmospheric conditions covering very-cold, very-dry, very-clear sky conditions to heavy overcast with traces of sleet. Spectral resolutions of 0.5 and 0,1 cm−1 were obtained with a radiometric accuracy of less than 0.5 K and a noise level on the order of 0.25 K rms. Overflights were made with the NASA ER2 high altitude research aircraft carrying a similar instrument [1, 2]. Aircraft and ground based LIDAR, radiosonde and other cloud physics experiments were also made at the same time to provide a data set complete enough to enable a much better understanding of the role of thin high clouds in the Earth's radiation balance. Measurements were made over the period from 10/24/86 to 11/21/86 in support of the NOAA/NASA/NSF project FIRE (First ISCCP Regional Experiment).</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="f">Springer Online Journal Archives 1860-2002</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">LaPorte, Daniel D.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Carpenter, James D.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Revercomb, Henry E.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">in</subfield><subfield code="t">Microchimica acta</subfield><subfield code="d">1937</subfield><subfield code="g">95(1988) vom: Jan./Juni, Seite 421-427</subfield><subfield code="w">(DE-627)NLEJ188993894</subfield><subfield code="w">(DE-600)1462152-6</subfield><subfield code="x">1436-5073</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:95</subfield><subfield code="g">year:1988</subfield><subfield code="g">month:01/06</subfield><subfield code="g">pages:421-427</subfield><subfield code="g">extent:7</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1007/BF01349801</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-SOJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">95</subfield><subfield code="j">1988</subfield><subfield code="c">1/6</subfield><subfield code="h">421-427</subfield><subfield code="g">7</subfield></datafield></record></collection>
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