The Aquarius/SAC-D joint international science mission, between the National Aeronautics and Space Administration (NASA) of United States and the Argentine Space Agency (Comision Nacional de Actividades Espaciales, CONAE), was launched on a polarorbiting satellite on June 10, 2011. This mission of discovery will provide measurements of the global sea surface salinity, which contributes to understanding climatic changes in the global water cycle and how these variations influence the general ocean circulation. The Microwave Radiometer (MWR), a three channel Dicke radiometer operating at 23.8 GHz H-Pol and 36.5 GHz V-& H-Pol provided by CONAE, will complement Aquarius (NASA’s L-band radiometer/scatterometer) by providing simultaneous spatially collocated environmental measurements such as water vapor, cloud liquid water, surface wind speed, rain rate and sea ice concentration. This dissertation focuses on the overall radiometric calibration of MWR instrument. Which means establishing a transfer function that relates the instrument output to the antenna brightness temperature (Tb). To achieve this goal, the dissertation describes a microwave radiative transfer model of the instrument and validates it using the laboratory and thermal-vacuum test data. This involves estimation of the losses and physical temperature profile in the path from the receiver to each antenna feed-horn for all the receivers. As the pre-launch laboratory tests can only provide a simulated environment which is very different from the operational environment in space, an on-orbit calibration of the instrument is very important. Inter-satellite radiometric cross-calibration of MWR using the Naval Research iii Laboratory’s multi-frequency polarimetric microwave radiometer, WindSat, on board the Coriolis satellite is also an important part of this dissertation. Cross-calibration between two different satellite instruments require normalization of Tb’s to account for the frequency and incidence angle difference between the instruments. Also inter-satellite calibration helps to determine accurate antenna pattern correction coefficients and other small instrument biases.

The removal of systematic brightness temperature (Tb) biases is necessary when producing decadal passive microwave data sets for weather and climate research. It is crucial to achieve Tb measurement consistency among all satellites in a constellation as well as to maintain sustained calibration accuracy over the lifetime of each satellite sensor. In-orbit inter-satellite radiometric calibration techniques provide a long term, group-wise solution; however, since radiometers operate at different frequencies and viewing angles, Tb normalizations are made before making intermediate comparisons of their near-simultaneous measurements. In this dissertation, a new approach is investigated to perform these normalizations from one satellite's measurements to another. It uses Taylor's series expansion around a source frequency to predict Tb of a desired frequency. The relationship between Tb's and frequencies are derived from simulations using an oceanic Radiative Transfer Model (RTM) over a wide variety of environmental conditions. The original RTM is built on oceanic radiative transfer theory. Refinements are made to the model by modifying and tuning algorithms for calculating sea surface emission, atmospheric emission and attenuations. Validations were performed with collocated WindSat measurements. This radiometric calibration approach is applied to establish an absolute brightness temperature reference using near-simultaneous pair-wise comparisons between a non-sun synchronous radiometer and two sun-synchronous polar-orbiting radiometers: the Tropical Rain Measurement Mission (TRMM) Microwave Imager (TMI), WindSat (on Coriolis) and Advanced Microwave Scanning Radiometer (AMSR) on Advanced Earth Observing System -II (ADEOSII), respectively. Collocated measurements between WindSat and TMI as well as between AMSR and TMI, within selected 10 weeks in 2003 for each pair, are collected, filtered and applied in the cross calibration. AMSR is calibrated to WindSat using TMI as a transfer standard. Accuracy prediction and error source analysis are discussed along with calibration results. This inter-satellite radiometric calibration approach provides technical support for NASA's Global Precipitation Mission which relies on a constellation of cooperative satellites with a variety of microwave radiometers to make global rainfall measurements.

Microwave radiometers are highly sensitive receivers capable of measuring low levels of natural blackbody microwave emissions. Remote sensing by satellite microwave radiometers flying on low-earth, polar orbiting, satellites can infer a variety of terrestrial and atmospheric geophysical parameters for scientific and operational applications, such as weather and climate prediction. The objective of this thesis is to provide realistic simulated ocean brightness temperatures for the 3-channel Microwave Radiometer (MWR), which will be launched in May 2010 on the joint NASA/CONAE Aquarius/SAC-D Mission. These data will be used for pre-launch geophysical retrieval algorithms development and validation testing. Analyses are performed to evaluate the proposed MWR measurement geometry and verify the requirements for spatial/temporal sampling. Finally, a preliminary study is performed for the post-launch inter-satellite radiometric calibration using the WindSat polarimetric radiometer on the Coriolis satellite.

A new method of power production, called pressurized oxy-fuel combustion, burns coal with CO2 and oxygen, rather than air, bringing us closer to the end goal of developing zero emission coal-fired utility boilers. However, high-pressure, high-temperature systems such as these are under-studied, and their behavior is difficult to measure. An accurate model for previously untested conditions requires data for validation. The heat release profile of flames and their radiative intensity is one of the key data sets required for model validation of an oxy-coal combustion system. A radiometer can be used to obtain the necessary radiative heat flux data. However, several studies show significant measurement errors of past radiometer designs. This work focuses on developing a narrow angle radiometer that can be used to describe radiative heat transfer from a pressurized oxy-coal flame. The sensitivity of the instrument to outside environmental influences is thoroughly examined, making it possible to obtain the axial radiative heat flux profile of the flame in a 100kW pressurized facility by accurately converting the measured quantities into radiative heat flux. Design aspects of the radiometer are chosen to improve the accuracy of radiative heat flux measurements as well as conform to the physical constraints of the 100kW pressurized facility. The radiometer is built with a 0.079-inch aperture, an 8.63-inch probe internally coated with high emissivity coating, four baffles spaced evenly down the length of the probe, no optic lens, a thermopile as the sensor, argon purge gas, and a water-cooled jacket. The radiometer has a viewing angle of 1.33 degrees. The instrument is calibrated with a black body radiator, and these calibration data are used in combination with radiation models to convert the radiometer signal in mV to radiative heat flux in kW/m2. Environmental factors affecting accuracy are studied. The results of the calibration data show that the radiometer measurements will produce a calculated heat flux that is accurate to within 5.98E-04 kW/m2.

No description available.

Accurate measurement of soil moisture (SM) has a significant impact on agricultural production, hydrological modeling, forestry, horticulture, waste management, and other environmental fields. Particularly in precision agriculture (PA), high spatiotemporal resolution information about surface SM is crucial. However, the use of invasive SM probes and other sensors is expensive and requires extensive manpower. Moreover, these intrusive techniques provide point measurements and are unsuitable for large agricultural fields. As an alternative, this dissertation explores the remote sensing of surface SM by utilizing the surface reflectivity estimated from global navigation satellite systems reflectometry (GNSS-R) data acquired through smartphones and off-the-shelf, cost-effective U-blox global navigation satellite systems (GNSS) receivers. To estimate surface reflectivity, the GNSS receivers are attached underneath a small unmanned aircraft system (UAS), which flies over agricultural fields. Additionally, this dissertation investigates a fully custom UAS-based dual-polarized L-band microwave radiometric measurement technique over agricultural areas to estimate surface brightness temperature (����). The radiometer measures surface emissivity as ����, allowing for the estimation of surface SM while considering the detection and removal of radio frequency interference (RFI) from the radiometric measurements. This radiometer processes the data in near real-time onboard the UAS, collecting raw in-phase and quadratic (I&Q) signals across the study field. This feature mitigates the RFI onboard and significantly reduces post-processing time. In summary, this study highlights the utilization of smartphones and semi-custom GNSS receivers in conjunction with UAS-based GNSS-R techniques and UAS-based L-band microwave radiometry for the estimation of surface reflectivity and ����. The radiometric measurement of surface emissivity is related to surface reflectivity through the relationship (Emissivity = 1 -Reflectivity).

Im Rahmen der Aktivitäten des ITG Fachausschusses 7.5 „Wellenausbreitung“ im VDE wird eine Fachtagung auf dem Gebiet Wellenausbreitung bei Funk-, Mikrowellensystemen und Navigation vom 4. – 5. Juli 2007 in Chemnitz abgehalten. Die Tagungsphilosophie betont den gemeinsamen Nenner der Wellenausbreitung in diversen Bereichen wie Mikrowellensensorik und Mikrowellensystemen. Bei der Fachtagung sind zusätzlich zu den Beiträgen der Fachausschussmitglieder, die zur Information über die Fachausschussaktivitäten dienen, auch Übersichtsvorträge und Diskussions-Sitzungen vorgesehen. Dem Leitthema zugeordnet, werden die folgenden Themen aus Fernerkundung, Kommunikation und Navigation besonders berücksichtigt: Mikrowellenausbreitung in der Kommunikation und Mikrowellensensorik - Gleichwellennetz - Digitale Übertragung - Mehrwegeausbreitung - Mehrfachnutzung - Innen-Gebäude-Übertragung - Mittelwellenausbreitung - Mobilfunk Nutzung und Anwendung in der Mikrowellensensorik - Radar-Polarimetrie - Bistatische und Multistatische Radarverfahren - Polarimetrische und Multistatische Interferometrie - Multiparameter-Wetterradar-Verfahren - Automobil- und Flugzeugradar - Kalibrierung - Biologische Effekte der EM-Strahlung:The ITG section 7.5 „Wellenausbreitung“ within the VDE (German Association for Electrical, Electronic & Information Technologies) is organising a conference on Wave Propagation in Communication, Microwave Systems and Navigation to be held during 4th and 5th of July 2007 in Chemnitz, Germany. The conference philosophy is to emphasize the commonalty between propagation aspects of microwave remote sensing sensors and microwave systems at large. In addition to the contributions from the members of ITG section 7.5, planned are review presentations and discussion sessions. The following topics of Remote Sensing, Communication and Navigation are eligible for presentation: Microwave Propagation in Communication and Microwave Sensors - Band Shared Broadcasting - Multi-Path Propagation - Digital Broadcasting - MIMO Systems and Reuse - Indoor Propagation - Medium Wave Propagation - Mobile Communication Applications of Microwave Sensors - Radar Polarimetry - Bistatic and Multistatic Radar - Polarimetric and Multistatic Interferometry - Multi-Parameter Weather Radar Systems - Automotive and Airborne Radars - System Calibration - Biological Effects of EM-Radiation

SMOS (Soil Moisture and Ocean Salinity) is ESA's Earth Explorer series satellite carrying the novel MIRAS (Microwave Imaging Radiometer with Aperture Synthesis) interferometric synthetic aperture radar. Its objective is monitoring and studying the planet's water cycle by following the changes in soil moisture levels and ocean surface salt concentrations on a global scale. The success of the mission calls for nearly uninterrupted operation of the science payload. However, the instrument experiences sporadically problems with its hardware, which cause losses of scientific data and may require intervention from ground to resolve. The geographical areas in which most of these anomalies occur, polar regions and the South-Atlantic anomaly, give cause to assume these problems are caused by charged particles in the planet's ionosphere. In this thesis, methods of predicting occurrence of hardware anomalies from indicators of Earth radiation environment are investigated.

L'altimétrie spatiale contribue majoritairement à la compréhension de la circulation océanique régionale et globale. Elle permet aujourd'hui de fournir une cartographie de la topographie océanique à des échelles spatiales et temporelles de plus en plus fines. Le passage du signal radar à travers la vapeur d'eau de l'atmosphère implique un retard de l'onde, qui nécessite d'être corrigé : c'est la correction troposphérique humide. Des méthodes statistiques sont actuellement utilisées pour estimer la correction troposphérique humide. Elles permettent d'inverser des mesures de températures de brillance fournies par un radiomètre couplé à l'altimètre sur une mission altimétrique, à deux ou trois fréquences proches de la bande d'absorption de la vapeur d'eau, à 22.235 GHz. Bien que ces algorithmes permettent d'estimer cette correction avec de faibles incertitudes en plein océan, des améliorations sont nécessaires pour réduire les erreurs dans les zones océaniques complexes, comme les régions d'upwelling, et sur les surfaces hétérogènes, comme en régions côtières, sur glace de mer, ou sur les eaux continentales. A ces fins, une approche variationnelle uni-dimensionnelle (1D-Var) est développée dans cette thèse. Elle permet de tenir compte de la physique de l'atmosphère et des variations de la surface dans l'environnement des mesures, pour estimer la correction troposphérique de manière globale, sur différents types de surface, dans le contexte des missions altimétriques actuelles, et futures, dont les technologies instrumentales évoluent. Une analyse fine des caractéristiques de l'approche 1D-Var, et de ses performances, permet de montrer l'apport et l'impact des différents paramètres en jeu sur les variables atmosphériques restituées, et la correction troposphérique humide estimée. Les performances du 1D-Var ainsi que ses limites sont évaluées pour l'estimation la correction troposphérique humide en plein océan, en conditions de ciel clair. L'apport des mesures de températures de brillance aux hautes fréquences, typiques des missions altimétriques futures, est également analysé. Leur potentiel est exploité dans le cadre de l'estimation de la correction troposphérique humide dans les régions côtières, où les mesures de températures de brillance sont contaminées par la présence de terre dans le signal. Enfin, une analyse des estimations des émissivités de surface, et de leurs variations sur la glace de mer, est proposée dans le cadre d'une étude préliminaire à l'estimation de la correction troposphérique humide, aux interfaces complexes mer/glace de mer, dans les régions polaires. / Space altimetry is one of the major contributors to the understanding of regional and global oceanic circulation. It currently enables to provide a map of ocean topography at higher temporal and spacial scales. A propagation delay of the altimeter signal along its path through atmospheric water vapor needs to be accounted for, and corresponds to the wet tropospheric correction. Statistical methods are currently used to estimate wet tropospheric correction. These methods are fed by brightness temperature measurements provided by a radiometer coupled to the altimeter, at two or three frequencies close to the water vapor absorption line, at 22.235 GHz. While these algorithms provide wet tropospheric correction with low uncertainties over open ocean, improvements are still needed to reduce higher uncertainties in complex oceanic areas, such as upwelling regions, and over heterogeneous surfaces, as coastal regions, sea ice or inland waters. To this end, a one-dimensional variational approach (1D-Var) is developed in the frame of this thesis. This approach accounts for atmospheric and surface variability in the surroundings of the measurements, to provide wet tropospheric correction estimates at a global scale, over various surfaces, in the context of both current and future altimetry missions, with improved instrumental technologies. We first analyze the characteristics of the 1D-Var approach and evaluate its performances. The contribution and impact of the different input parameters on retrieved atmospheric variables and wet tropospheric correction are shown through this analysis. The potential and limits of the 1D-Var approach to retrieve wet tropospheric correction over open ocean, for clear sky conditions, are evaluated. The contribution of high frequencies, typical to future altimetry missions, is also analyzed. It is fully exploited to retrieve wet tropospheric correction over coastal areas, where land contamination occurs within brightness temperature measurements. A preliminary analysis of surface emissivity estimates and their variability over sea ice is also undertaken, in the frame of the 1D-Var estimation of wet tropospheric correction over sea ice/open sea transition surfaces, in polar areas.

The ITG section 7.5 "Wellenausbreitung" within the VDE (German Association for Electrical, Electronic & Information Technologies) organised a conference on Wave Propagation in Communication, Microwave Systems and Navigation which was held during 25th - 27th of November 2009 in Chemnitz, Germany. The conference philosophy is to emphasize the commonalty between propagation aspects of microwave remote sensing sensors and microwave systems at large. The following topics of Remote Sensing, Communication and Navigation are eligible for presentation: Microwave Propagation in Communication and Microwave Sensors - Satellite Communications - Multi-Path Propagation - Indoor Propagation - Digital Broadcast Planning - MIMO Systems and Reuse - Ionospheric Propagation - Urban Communication - Microwave Measurements in Propagation Applications of Microwave Sensors - Radar Polarimetry - Bistatic and Multistatic Radar - Polarimetric and Multistatic Interferometry - Multi-Parameter Weather Radar Systems - Automotive and Airborne Radars - System Calibration - Biological Effects of EM-Radiation - Wave Modulation Remote Sensing Radars Antenna Design and Measurements / Im Rahmen der Aktivitäten des ITG-Fachausschusses 7.5 "Wellenausbreitung" im VDE wurde eine Fachtagung auf dem Gebiet Wellenausbreitung bei Funk-, Mikrowellensystemen und Navigation vom 25. - 27. November 2009 in Chemnitz abgehalten. Die Tagungsphilosophie betont den gemeinsamen Nenner der Wellenausbreitung in diversen Bereichen wie Mikrowellensensorik und Mikrowellensystemen. Dem Leitthema zugeordnet, werden die folgenden Themen aus Fernerkundung, Kommunikation und Navigation besonders berücksichtigt. Mikrowellenausbreitung in der Kommunikation und Mikrowellensensorik - Satellitenkommunikation - Mehrwegeausbreitung - Innen-Gebäude-Übertragung - Frequenzplanung für den digitalen Rundfunk - MIMO Systeme - Wellenausbreitung in der Ionosphäre - urbane Kommunikation - Mikrowellenmessungen der Wellenausbreitung Nutzung und Anwendung in der Mikrowellensensorik - Radar-Polarimetrie - Bistatische und Multistatische Radarverfahren - Polarimetrische und Multistatische Interferometrie - Multiparameter-Wetterradar-Verfahren - Automobil- und Flugzeugradar - Systemkalibrierung - Biologische Effekte der EM-Strahlung - Antennenentwicklung und -messungen für wellenmodulierte Fernerkundungsradare