Relevant bibliographies by topics / Satellite-borne radiometers

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Satellite-borne radiometers'

Author: Grafiati
Published: 4 June 2021
Last updated: 5 February 2022

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Journal articles on the topic "Satellite-borne radiometers"

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PECKHAM, G. E. "The vertical resolution of satellite borne radiometers for atmospheric measurements." International Journal of Remote Sensing 16, no. 8 (1995): 1557–69. http://dx.doi.org/10.1080/01431169508954494.

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Zeng, Xiping, Gail Skofronick-Jackson, Lin Tian, Amber E. Emory, William S. Olson, and Rachael A. Kroodsma. "Analysis of the Global Microwave Polarization Data of Clouds." Journal of Climate 32, no. 1 (2018): 3–13. http://dx.doi.org/10.1175/jcli-d-18-0293.1.

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Abstract Information about the characteristics of ice particles in clouds is necessary for improving our understanding of the states, processes, and subsequent modeling of clouds and precipitation for numerical weather prediction and climate analysis. Two NASA passive microwave radiometers, the satellite-borne Global Precipitation Measurement (GPM) Microwave Imager (GMI) and the aircraft-borne Conical Scanning Millimeter-Wave Imaging Radiometer (CoSMIR), measure vertically and horizontally polarized microwaves emitted by clouds (including precipitating particles) and Earth’s surface below. In
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Guan, Ji-Ping, Yan-Tong Yin, Li-Feng Zhang, Jing-Nan Wang, and Ming-Yang Zhang. "Comparison Analysis of Total Precipitable Water of Satellite-Borne Microwave Radiometer Retrievals and Island Radiosondes." Atmosphere 10, no. 7 (2019): 390. http://dx.doi.org/10.3390/atmos10070390.

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Total precipitable water (TPW) of satellite-borne microwave radiometer retrievals is compared with the data that were collected from 49 island radiosonde stations for the period 2007–2015. Great consistency was found between TPW measurements made by radiosonde and eight satellite-borne microwave radiometers, including SSMI-F13, SSMI-F14, SSMIS-F16, SSMIS-F17, AMSR-E, AMSR-2, GMI, and WindSat. Mean values of the TPW differences for eight satellites ranged from −0.51 to 0.38mm, both root mean square errors and standard deviations were around 3mm, and all of the correlation coefficients between s
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Tamura, Takeshi, Kay I. Ohshima, Jan L. Lieser, et al. "Helicopter-borne observations with portable microwave radiometer in the Southern Ocean and the Sea of Okhotsk." Annals of Glaciology 56, no. 69 (2015): 436–44. http://dx.doi.org/10.3189/2015aog69a621.

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AbstractAccurately measuring and monitoring the thickness distribution of thin ice is crucial for accurate estimation of ocean–atmosphere heat fluxes and rates of ice production and salt flux in ice-affected oceans. Here we present results from helicopter-borne brightness temperature (TB) measurements in the Southern Ocean in October 2012 and in the Sea of Okhotsk in February 2009 carried out with a portable passive microwave (PMW) radiometer operating at a frequency of 36 GHz. The goal of these measurements is to aid evaluation of a satellite thin-ice thickness algorithm which uses data from
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Dietrich, S., D. Casella, F. Di Paola, M. Formenton, A. Mugnai, and P. Sanò. "Lightning-based propagation of convective rain fields." Natural Hazards and Earth System Sciences 11, no. 5 (2011): 1571–81. http://dx.doi.org/10.5194/nhess-11-1571-2011.

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Abstract. This paper describes a new multi-sensor approach for continuously monitoring convective rain cells. It exploits lightning data from surface networks to propagate rain fields estimated from multi-frequency brightness temperature measurements taken by the AMSU/MHS microwave radiometers onboard NOAA/EUMETSAT low Earth orbiting operational satellites. Specifically, the method allows inferring the development (movement, morphology and intensity) of convective rain cells from the spatial and temporal distribution of lightning strokes following any observation by a satellite-borne microwave
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Ryan, Niall J., Kaley A. Walker, Uwe Raffalski, Rigel Kivi, Jochen Gross, and Gloria L. Manney. "Ozone profiles above Kiruna from two ground-based radiometers." Atmospheric Measurement Techniques 9, no. 9 (2016): 4503–19. http://dx.doi.org/10.5194/amt-9-4503-2016.

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Abstract. This paper presents new atmospheric ozone concentration profiles retrieved from measurements made with two ground-based millimetre-wave radiometers in Kiruna, Sweden. The instruments are the Kiruna Microwave Radiometer (KIMRA) and the Millimeter wave Radiometer 2 (MIRA 2). The ozone concentration profiles are retrieved using an optimal estimation inversion technique, and they cover an altitude range of ∼ 16–54 km, with an altitude resolution of, at best, 8 km. The KIMRA and MIRA 2 measurements are compared to each other, to measurements from balloon-borne ozonesonde measurements at S
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Fan, Xia, and Chen. "Intercomparison of Multiple Satellite Aerosol Products against AERONET over the North China Plain." Atmosphere 10, no. 9 (2019): 480. http://dx.doi.org/10.3390/atmos10090480.

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In this study, using Aerosol Robotic Network aerosol optical depth (AOD) products at three stations in the North China Plain (NCP)—a heavily polluted region in China—the AOD products from six satellite-borne radiometers: the Moderate Resolution Imagining Spectroradiometer (MODIS), the Multiangle Imaging Spectroradiometer (MISR), Ozone Mapping Imaging (OMI), the Visible Infrared Imaging Radiometer (VIIRS), the Sea-Viewing Wide Field-of-View Sensor (SeaWiFS), and Polarization and Directionality of the Earth’s Reflectances (POLDER), were thoroughly validated, shedding new light on their advantage
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Kubota, Takuji, Shoichi Shige, Hiroshi Hashizume, et al. "Global Precipitation Map Using Satellite-Borne Microwave Radiometers by the GSMaP Project: Production and Validation." IEEE Transactions on Geoscience and Remote Sensing 45, no. 7 (2007): 2259–75. http://dx.doi.org/10.1109/tgrs.2007.895337.

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9

Gao, Qidong, Sheng Wang, and Xiaofeng Yang. "Estimation of Surface Air Specific Humidity and Air–Sea Latent Heat Flux Using FY-3C Microwave Observations." Remote Sensing 11, no. 4 (2019): 466. http://dx.doi.org/10.3390/rs11040466.

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Latent heat flux (LHF) plays an important role in the global hydrological cycle and is therefore necessary to understand global climate variability. It has been reported that the near-surface specific humidity is a major source of error for satellite-derived LHF. Here, a new empirical model relating multichannel brightness temperatures ( T B ) obtained from the Fengyun-3 (FY-3C) microwave radiometer and sea surface air specific humidity ( Q a ) is proposed. It is based on the relationship between T B , Q a , sea surface temperature (SST), and water vapor scale height. Compared with in situ dat
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Medaglia, C. M., C. Adamo, F. Baordo, et al. "Comparing microphysical/dynamical outputs by different cloud resolving models: impact on passive microwave precipitation retrieval from satellite." Advances in Geosciences 2 (May 7, 2005): 195–99. http://dx.doi.org/10.5194/adgeo-2-195-2005.

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Abstract. Mesoscale cloud resolving models (CRM's) are often utilized to generate consistent descriptions of the microphysical structure of precipitating clouds, which are then used by physically-based algorithms for retrieving precipitation from satellite-borne microwave radiometers. However, in principle, the simulated upwelling brightness temperatures (TB's) and derived precipitation retrievals generated by means of different CRM's with different microphysical assumptions, may be significantly different even when the models simulate well the storm dynamical and rainfall characteristics. In
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Dissertations / Theses on the topic "Satellite-borne radiometers"

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Jung, Fan. "Satellite measurements of surface temperatures." Thesis, University of Oxford, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.308756.

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Werrett, Stephen T. R. "Aspects of the design of a satellite borne infra-red radiometer." Thesis, University of Oxford, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303618.

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Mason, Graeme. "Test and calibration of the Along Track Scanning Radiometer, a satellite-borne infrared radiometer designed to measure sea surface temperature." Thesis, University of Oxford, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.293406.

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Books on the topic "Satellite-borne radiometers"

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United States. National Aeronautics and Space Administration., ed. EOS/AMSU-A NASA/Aerojet Interface Meeting: 11 May 1993. GenCorp Aerojet, 1993.

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EOS/AMSU-A NASA/Aerojet Interface Meeting: 11 May 1993. GenCorp Aerojet, 1993.

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EOS/AMSU-A NASA/Aerojet Interface Meeting: 11 May 1993. GenCorp Aerojet, 1993.

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United States. National Aeronautics and Space Administration., ed. EOS/AMSU-A NASA/Aerojet Interface Meeting: 11 May 1993. GenCorp Aerojet, 1993.

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5

H, Staelin David, and United States. National Aeronautics and Space Administration., eds. Comparative analysis of alternate MHS configurations. National Aeronautics and Space Administration, 1995.

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H, Staelin David, and United States. National Aeronautics and Space Administration., eds. Comparative analysis of alternate MHS configurations. National Aeronautics and Space Administration, 1995.

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H, Staelin David, and United States. National Aeronautics and Space Administration., eds. Comparative analysis of alternate MHS configurations. National Aeronautics and Space Administration, 1995.

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Center, Langley Research, ed. A conceptual thermal design study of an electronically scanned thinned array radiometer. National Aeronautics and Space Administration, Langley Research Center, 1995.

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Book chapters on the topic "Satellite-borne radiometers"

1

Brock, Fred V., and Scott J. Richardson. "Upper Air Measurements." In Meteorological Measurement Systems. Oxford University Press, 2001. http://dx.doi.org/10.1093/oso/9780195134513.003.0014.

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Measurements of atmospheric properties become progressively more difficult with altitude above the surface of the earth, and even surface measurements are difficult over the oceans. First balloons, then airplanes and rockets, were used to carry instruments aloft to make in-situ measurements. Now remote sensors, both ground-based and satellite-borne, are used to monitor the atmosphere. In this context, upper air means all of the troposphere above the first hundred meters or so and, in some cases, the stratosphere. There are many uncertainties associated with remote sensing, so there is a demand for in-situ sensors to verify remote measurements. In addition, the balloon- borne instrument package is relatively inexpensive. However, it should be noted that cost is a matter of perspective; a satellite with its instrumentation, ground station, etc. may be cost-effective when the mission is to make measurements all over the world with good space and time resolution, as synoptic meteorology demands. Upper air measurements of pressure, temperature, water vapor, and winds can be made using in-situ instrument packages (carried aloft by balloons, rockets, or airplanes) and by remote sensors. Remote sensors can be classified as active (energy emitters like radar or lidar) or passive (receiving only, like microwave radiometers), and by whether they “look” up from the ground or down from a satellite. Remote sensors are surveyed briefly before discussing in-situ instruments. Profiles of temperature, humidity, density, etc. can be estimated from satellites using multiple narrow-band radiometers. These are passive sensors that measure longwave radiation upwelling from the atmosphere. For example, temperature profiles can be estimated from satellites by measuring infrared radiation emitted by CO2 (bands around 5000 μm) and O2 (bands around 3.4μm and 15μm) in the atmosphere. Winds can be estimated from cloud movements or by using the Doppler frequency shift due to some component of the atmosphere being carried along with the wind. An active sensor (radar) is used to estimate precipitation and, if it is a Doppler radar, determine winds. The great advantage of satellite-borne instruments is that they can cover the whole earth with excellent spatial resolution.
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2

Donlon, Craig J., Peter J. Minnett, Nigel Fox, and Werenfrid Wimmer. "Strategies for the Laboratory and Field Deployment of Ship-Borne Fiducial Reference Thermal Infrared Radiometers in Support of Satellite-Derived Sea Surface Temperature Climate Data Records." In Experimental Methods in the Physical Sciences. Elsevier, 2014. http://dx.doi.org/10.1016/b978-0-12-417011-7.00018-0.

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Conference papers on the topic "Satellite-borne radiometers"

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Burrage, Derek, Joel Wesson, Paul Hwang, and David Wang. "Performance of roughness correction models for retrieval of Sea Surface Salinity from air- and satellite-borne L-band radiometers." In IGARSS 2010 - 2010 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2010. http://dx.doi.org/10.1109/igarss.2010.5654454.

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Manalo, Natividad D., and G. Louis Smith. "Spatial sampling errors for a satellite-borne scanning radiometer." In Orlando '91, Orlando, FL, edited by Bruce W. Guenther. SPIE, 1991. http://dx.doi.org/10.1117/12.46705.

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Maeda, Takashi, and Tadashi Takano. "Approach for volcanic surveillance using satellite-borne microwave radiometer data." In IGARSS 2010 - 2010 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2010. http://dx.doi.org/10.1109/igarss.2010.5652610.

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Maeda, Takashi, and Tadashi Takano. "Detection of microwave signals associated with rock failures in an earthquake from satellite-borne microwave radiometer data." In 2009 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2009. http://dx.doi.org/10.1109/igarss.2009.5418159.

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