Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies
Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based m...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Nagasaki, T. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science+Business Media New York 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Journal of low temperature physics - Springer US, 1969, 184(2015), 3-4 vom: 29. Dez., Seite 674-679 |
|---|---|
| Übergeordnetes Werk: |
volume:184 ; year:2015 ; number:3-4 ; day:29 ; month:12 ; pages:674-679 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10909-015-1412-9 |
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| Katalog-ID: |
OLC2036826970 |
|---|
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| 520 | |a Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. | ||
| 650 | 4 | |a Radiometer | |
| 650 | 4 | |a Meteorology | |
| 650 | 4 | |a Precipitable water vapor | |
| 650 | 4 | |a Oxygen | |
| 650 | 4 | |a Atmospheric radiation | |
| 700 | 1 | |a Araki, K. |4 aut | |
| 700 | 1 | |a Ishimoto, H. |4 aut | |
| 700 | 1 | |a Kominami, K. |4 aut | |
| 700 | 1 | |a Tajima, O. |4 aut | |
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10.1007/s10909-015-1412-9 doi (DE-627)OLC2036826970 (DE-He213)s10909-015-1412-9-p DE-627 ger DE-627 rakwb eng 530 VZ Nagasaki, T. verfasserin aut Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media New York 2015 Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. Radiometer Meteorology Precipitable water vapor Oxygen Atmospheric radiation Araki, K. aut Ishimoto, H. aut Kominami, K. aut Tajima, O. aut Enthalten in Journal of low temperature physics Springer US, 1969 184(2015), 3-4 vom: 29. Dez., Seite 674-679 (DE-627)129546267 (DE-600)218311-0 (DE-576)014996642 0022-2291 nnns volume:184 year:2015 number:3-4 day:29 month:12 pages:674-679 https://doi.org/10.1007/s10909-015-1412-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_22 GBV_ILN_70 GBV_ILN_170 GBV_ILN_2185 GBV_ILN_4126 GBV_ILN_4323 AR 184 2015 3-4 29 12 674-679 |
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10.1007/s10909-015-1412-9 doi (DE-627)OLC2036826970 (DE-He213)s10909-015-1412-9-p DE-627 ger DE-627 rakwb eng 530 VZ Nagasaki, T. verfasserin aut Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media New York 2015 Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. Radiometer Meteorology Precipitable water vapor Oxygen Atmospheric radiation Araki, K. aut Ishimoto, H. aut Kominami, K. aut Tajima, O. aut Enthalten in Journal of low temperature physics Springer US, 1969 184(2015), 3-4 vom: 29. Dez., Seite 674-679 (DE-627)129546267 (DE-600)218311-0 (DE-576)014996642 0022-2291 nnns volume:184 year:2015 number:3-4 day:29 month:12 pages:674-679 https://doi.org/10.1007/s10909-015-1412-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_22 GBV_ILN_70 GBV_ILN_170 GBV_ILN_2185 GBV_ILN_4126 GBV_ILN_4323 AR 184 2015 3-4 29 12 674-679 |
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10.1007/s10909-015-1412-9 doi (DE-627)OLC2036826970 (DE-He213)s10909-015-1412-9-p DE-627 ger DE-627 rakwb eng 530 VZ Nagasaki, T. verfasserin aut Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media New York 2015 Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. Radiometer Meteorology Precipitable water vapor Oxygen Atmospheric radiation Araki, K. aut Ishimoto, H. aut Kominami, K. aut Tajima, O. aut Enthalten in Journal of low temperature physics Springer US, 1969 184(2015), 3-4 vom: 29. Dez., Seite 674-679 (DE-627)129546267 (DE-600)218311-0 (DE-576)014996642 0022-2291 nnns volume:184 year:2015 number:3-4 day:29 month:12 pages:674-679 https://doi.org/10.1007/s10909-015-1412-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_22 GBV_ILN_70 GBV_ILN_170 GBV_ILN_2185 GBV_ILN_4126 GBV_ILN_4323 AR 184 2015 3-4 29 12 674-679 |
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10.1007/s10909-015-1412-9 doi (DE-627)OLC2036826970 (DE-He213)s10909-015-1412-9-p DE-627 ger DE-627 rakwb eng 530 VZ Nagasaki, T. verfasserin aut Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media New York 2015 Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. Radiometer Meteorology Precipitable water vapor Oxygen Atmospheric radiation Araki, K. aut Ishimoto, H. aut Kominami, K. aut Tajima, O. aut Enthalten in Journal of low temperature physics Springer US, 1969 184(2015), 3-4 vom: 29. Dez., Seite 674-679 (DE-627)129546267 (DE-600)218311-0 (DE-576)014996642 0022-2291 nnns volume:184 year:2015 number:3-4 day:29 month:12 pages:674-679 https://doi.org/10.1007/s10909-015-1412-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_22 GBV_ILN_70 GBV_ILN_170 GBV_ILN_2185 GBV_ILN_4126 GBV_ILN_4323 AR 184 2015 3-4 29 12 674-679 |
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10.1007/s10909-015-1412-9 doi (DE-627)OLC2036826970 (DE-He213)s10909-015-1412-9-p DE-627 ger DE-627 rakwb eng 530 VZ Nagasaki, T. verfasserin aut Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media New York 2015 Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. Radiometer Meteorology Precipitable water vapor Oxygen Atmospheric radiation Araki, K. aut Ishimoto, H. aut Kominami, K. aut Tajima, O. aut Enthalten in Journal of low temperature physics Springer US, 1969 184(2015), 3-4 vom: 29. Dez., Seite 674-679 (DE-627)129546267 (DE-600)218311-0 (DE-576)014996642 0022-2291 nnns volume:184 year:2015 number:3-4 day:29 month:12 pages:674-679 https://doi.org/10.1007/s10909-015-1412-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_22 GBV_ILN_70 GBV_ILN_170 GBV_ILN_2185 GBV_ILN_4126 GBV_ILN_4323 AR 184 2015 3-4 29 12 674-679 |
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Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies |
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Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies |
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Nagasaki, T. |
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Journal of low temperature physics |
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Journal of low temperature physics |
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2015 |
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Nagasaki, T. Araki, K. Ishimoto, H. Kominami, K. Tajima, O. |
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184 |
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Nagasaki, T. |
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10.1007/s10909-015-1412-9 |
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530 |
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monitoring system for atmospheric water vapor with a ground-based multi-band radiometer: meteorological application of radio astronomy technologies |
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Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies |
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Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. © Springer Science+Business Media New York 2015 |
| abstractGer |
Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. © Springer Science+Business Media New York 2015 |
| abstract_unstemmed |
Abstract High-resolution estimation of thermodynamic properties in the atmosphere can help to predict and mitigate meteorological disasters, such as local heavy rainfall and tornadic storms. For the purposes of short-term forecasting and nowcasting of severe storms, we propose a novel ground-based measurement system, which observes the intensity of atmospheric radiation in the microwave range. Our multi-band receiver system is designed to identify a rapid increase in water vapor before clouds are generated. At frequencies between 20 and 30 GHz, our system simultaneously measures water vapor as a broad absorption peak at 22 GHz as well as cloud liquid water. Another band at 50–60 GHz provides supplementary information from oxygen radiation to give vertical profiles of physical temperature. For the construction of this cold receiver system, novel technologies originally developed for observations of cosmic microwave background radiation were applied. The input atmospheric signal is amplified by a cold low-noise amplifier maintained below 10 K, while the spectrum of this amplified signal is measured using a signal analyzer under ambient conditions. The cryostat also contains a cold black body at 40 K to act as a calibration signal. This calibration signal is transported to each of the receivers via a wire grid. We can select either the atmospheric signal or the calibration signal by changing the orientation of this wire. Each receiver can be calibrated using this setup. Our system is designed to be compact ($$<$$1 m$$^{3}$$), with low power consumption ($$\sim $$1.5 kW). Therefore, it is easy to deploy on top of high buildings, mountains, and ship decks. © Springer Science+Business Media New York 2015 |
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Monitoring System for Atmospheric Water Vapor with a Ground-Based Multi-Band Radiometer: Meteorological Application of Radio Astronomy Technologies |
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