The Microwave Radiometer Technology Acceleration Cubesat
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New Capabilities for All-Weather Microwave Atmospheric Sensing Using Cubesats and Constellations
SSC18-II-07 New Capabilities for All-Weather Microwave Atmospheric Sensing Using CubeSats and Constellations W. Blackwell, K. Clark, D. Cousins, D. Crompton, A. Cunningham, M. Diliberto, L. Fuhrman, R. Leslie, I. Osaretin, and S. Michael MIT Lincoln Laboratory [email protected] ABSTRACT Three MIT Lincoln Laboratory nanosatellite missions flying microwave radiometers for high-resolution atmospheric sensing are in varying stages of development. Microwave instrumentation is particularly well suited for implementation on a very small satellite, as the sensor requirements for power, pointing, and spatial resolution (aperture size) can be accommodated by a nanosatellite platform. The Microsized Microwave Atmospheric Satellite Version 2a (MicroMAS-2a), launched on January 11, 2018 and has demonstrated temperature sounding using channels near 118 GHz and humidity sounding using channels near 183 GHz. A second MicroMAS-2 flight unit (MicroMAS-2b) will be launched in Fall 2018 as part of ELANA-XX. The Time-Resolved Observations of Precipitation structure and storm Intensity with a Constellation of Smallsats (TROPICS) mission was selected by NASA in 2016 as part of the Earth Venture–Instrument (EVI-3) program. The overarching goal for TROPICS is to provide nearly all-weather observations of 3-D temperature and humidity, as well as cloud ice and precipitation horizontal structure, at high temporal resolution to conduct high-value science investigations of tropical cyclones. TROPICS will provide rapid-refresh microwave measurements (median refresh rate of approximately 40 minutes for the baseline mission) over the tropics that can be used to observe the thermodynamics of the troposphere and precipitation structure for storm systems at the mesoscale and synoptic scale over the entire storm lifecycle. -
Passive Microwave Radiometer Channel Selection Based on Cloud and Precipitation Information Content Estimation
475 Passive Microwave Radiometer Channel Selection Based on Cloud and Precipitation Information Content Estimation Sabatino Di Michele and Peter Bauer Research Department Submitted to Q. J. Royal Meteor. Soc. July 2005 Series: ECMWF Technical Memoranda A full list of ECMWF Publications can be found on our web site under: http://www.ecmwf.int/publications/ Contact: [email protected] c Copyright 2005 European Centre for Medium-Range Weather Forecasts Shinfield Park, Reading, RG2 9AX, England Literary and scientific copyrights belong to ECMWF and are reserved in all countries. This publication is not to be reprinted or translated in whole or in part without the written permission of the Director. Appropriate non-commercial use will normally be granted under the condition that reference is made to ECMWF. The information within this publication is given in good faith and considered to be true, but ECMWF accepts no liability for error, omission and for loss or damage arising from its use. Microwave Channel Selection from Precipitation Information Content Abstract The information content of microwave frequencies between 5 and 200 GHz for rain, snow and cloud wa- ter retrievals over ocean and land surfaces was evaluated using optimal estimation theory. The study was based on large datasets representative of summer and winter meteorological conditions over North Amer- ica, Europe, Central Africa, South America and the Atlantic obtained from short-range forecasts with the operational ECMWF model. The information content was traded off against noise that is mainly produced by geophysical variables such as surface emissivity, land surface skin temperature, atmospheric temperature and moisture. The estimation of the required error statistics was based on ECMWF model forecast error statistics. -
Instruments for Earth Science Measurements
NASA SBIR 2004 Phase I Solicitation E1 Instruments for Earth Science Measurements NASA's Earth Science Enterprise (ESE) is studying how our global environment is changing. Using the unique perspective available from space and airborne platforms, NASA is observing, documenting, and assessing large- scale environmental processes with emphasis on atmospheric composition, climate, carbon cycle and ecosystems, the Earth’s surface and interior, the water and energy cycles, and weather. A major objective of the ESE instrument development programs is to implement science measurement capabilities with small or more affordable spacecraft so development programs can meet multiple mission needs and therefore, make the best use of limited resources. The rapid development of small, low cost remote sensing and in situ instruments is essential to achieving this objective. Consequently, the objective of the Instruments for Earth Science Measurements SBIR topic is to develop and demonstrate instrument component and subsystem technologies that reduce the risk, cost, size, and development time of Earth observing instruments, and enable new Earth observation measurements. The following subtopics are concomitant with this objective and are organized by measurement technique. Subtopics E1.01 Passive Optics Lead Center: LaRC Participating Center(s): ARC, GSFC The following technologies are of interest to NASA in the remote sensing subtopic “passive optics.” Passive optical remote sensing generally requires that deployed devices have large apertures and large throughput. NASA is interested primarily in instrument technologies suitable for aircraft or space flight platforms, and these inherently also prefer low mass, low power, fast measurement times, and a high degree of robustness to survive vibrations in flight or at launch. -
N€WS 'RELEASE NATIONAL AERONAUTICS and SPACE Admln ISTRATION 400 MARYLAND AVENUE, SW, WASHINGTON 25, D.C
https://ntrs.nasa.gov/search.jsp?R=19630002483 2020-03-11T16:50:02+00:00Z b " N€WS 'RELEASE NATIONAL AERONAUTICS AND SPACE ADMlN ISTRATION 400 MARYLAND AVENUE, SW, WASHINGTON 25, D.C. TELEPHONES WORTH 2-4155-WORTH. 3-1110 RELEASE NO. 62-182 MARINER SPACECRAFT Mariner 2, the second of a series of spacecraft designed for planetary exploration,- will be launched within a few days (no earlier than August 17) from the Atlantic Missile Range, Cape Canaveral, Florida, by the National Aeronautics and Space Administration. Mariner 1, launched at 4:21 a.m. (EST) on July 22, 1962 from AMR, was destroyed by the Range Safety Officer after about 290 seconds of flight because of a deviation from the planned flight path. Measures have been taken to correct the difficulties experienced in the Mariner 1 launch. These measures include a more rigorous checkout of the Atlas rate beacon and revision of the data editing equation. The data editing equation Is designed as a guard against acceptance of faulty databy the ground guidance equipment. The Mariner 2 spacecraft and its mission are identical to the first Mariner. Mariner 2 will carry six experiments. Two of these instruments, infrared and microwave radiometers, will make measurements at close range as Mariner 2 flys by Venus and communicate this in€ormation over an interplanetary distance of 36 million miles, Four other experiments on the spacecraft -- a magnetometer, ion chamber and particle flux detector, cosmic dust detector and solar plasma spectrometer -- will gather Information on interplantetary phenomena during the trip to Venus and in the vicinity of the planet. -
An Assessment of Rain “Contamination” in ARM Two
An assessment of rain “contamination” in ARM two-channel microwave radiometer measurements Roger Marchand1, Casey Wall1*, Wei Zhao1 and Maria Cadeddu2 1University of Washington, 2Argonne National Laboratory, *Presenting Author Case 1 Case 3 Motivation! ? !! ✔ ? � ✔ 5000 wet-window flag (open/covered) ! Microwave radiometers (MWRs) are the most commonly used and wet-window flag (open/covered) 1500 3000 accurate instruments ARM has to retrieve cloud liquid water path. open MWR open MWR Unfortunately, MWR data are not easily used in precipitating conditions. 1000 500 There are two reasons for this:" 5000 ) ) 2 1500 " 2 1. The measurements are “contaminated” by water on the MWR radome." 3000 covered! covered! MWR MWR 2. Precipitating particles can scatter microwave radiation, yet traditional 1000 500 MWR retrievals neglect scattering." 5000 " 1500 "We designed an experiment that alleviates the “wet radome” problem. 3000 1000 500 5000 The Experiment! 1500 !! 3000 500 ! Two MWRs were operated side by side in a “scanning” or tip-cal mode. Path (g/m Water Liquid 1000 Liquid Water Path (g/m Path Water Liquid One MWR was placed under a cover that kept the radome dry while still 5000 permitting measurements away from zenith (photograph below). The 1500 other MWR was operated normally, with the radome exposed to the sky. 3000 We refer to these as the “covered” and “open” MWRs, respectively. 1000 500 Coincident measurements from the 17.8 18.2 18.6 19 19.4 19.8 covered and open MWRs are 17.5 18 18.5 19 compared to estimate contamination Hours (UTC) Hours (UTC) Case 2 due to a wet radome. -
Evidence of Diurnal Variations of Titan's Near-Surface Temperature
EPSC Abstracts Vol. 14, EPSC2020-618, 2020 https://doi.org/10.5194/epsc2020-618 Europlanet Science Congress 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Evidence of diurnal variations of Titan’s near-surface temperature and of a cooling effect of the northern seas from the Cassini radar/radiometer Alice Le Gall1,2, Léa Bonnefoy1,3, Robin Sultana4, Michael Janssen5, Ralph Lorenz6, and Tetsuya Tokano7 1LATMOS/IPSL, UVSQ, Université Paris-Saclay, CNRS, Sorbonne Université 2Institut Universitaire de France (IUF), Paris, France 3LESIA, Observatoire de Paris/Université PSL, CNRS, Sorbonne Université, Université Paris-Diderot, Meudon, France 4IPAG, Université Grenoble Alpes, CNRS, Grenoble, France 5Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA 6Johns Hopkins Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD, USA 7Institut für Geophysik und Meteorologie, Universität zu Köln, Cologne, Germany At first order, the physical temperature of Titan’s surface can be regarded as nearly constant and predictable. Due to the low incident solar flux reaching its surface (1/1000 of what Earth receives) and the high thermal inertia of its atmosphere, diurnal, seasonal (including latitudinal) and altitudinal variations of temperature are limited as well as the effect of surface albedo (Lorenz et al., 1999). Voyager 1 radio-occultation measurements indeed show no diurnal effect and point to lapse rates in the lower atmosphere smaller than 1.5 K/km (McKay et al 1997). Voyager infrared observations indicate a pole-to-equator temperature contrast of 2-3 K (Flasar et al., 1981; 1998). The Cassini mission (2004-2017) somewhat confirmed these predictions and first measurements. -
Impact of Assimilating Ground-Based Microwave Radiometer Data on the Precipitation Bifurcation Forecast: a Case Study in Beijing
atmosphere Article Impact of Assimilating Ground-Based Microwave Radiometer Data on the Precipitation Bifurcation Forecast: A Case Study in Beijing Yajie Qi 1,2, Shuiyong Fan 1,*, Jiajia Mao 3, Bai Li 3, Chunwei Guo 1 and Shuting Zhang 1 1 Institute of Urban Meteorology, China Meteorological Administration, Beijing 100089, China; [email protected] (Y.Q.); [email protected] (C.G.); [email protected] (S.Z.) 2 Key Laboratory for Cloud Physics of China Meteorological Administration, Beijing 100081, China 3 Meteorological Observation Center of China Meteorological Administration, Beijing 100081, China; [email protected] (J.M.); [email protected] (B.L.) * Correspondence: [email protected] Abstract: In this study, the temperature and relative humidity profiles retrieved from five ground- based microwave radiometers in Beijing were assimilated into the rapid-refresh multi-scale analysis and prediction system-short term (RMAPS-ST). The precipitation bifurcation prediction that occurred in Beijing on 4 May 2019 was selected as a case to evaluate the impact of their assimilation. For this purpose, two experiments were set. The Control experiment only assimilated conventional observations and radar data, while the microwave radiometers profilers (MWRPS) experiment assimilated conventional observations, the ground-based microwave radiometer profiles and radar data into the RMAPS-ST model. The results show that in comparison with the Control test, the Citation: Qi, Y.; Fan, S.; Mao, J.; Li, B.; MWRPS test made reasonable adjustments for the thermal conditions in time, better reproducing Guo, C.; Zhang, S. Impact of the weak heat island phenomenon in the observation prior to the rainfall. Thus, assimilating Assimilating Ground-Based MWRPS improved the skills of the precipitation forecast in both the distribution and the intensity of Microwave Radiometer Data on the rainfall precipitation, capable of predicting the process of belt-shaped radar echo splitting and the Precipitation Bifurcation Forecast: A precipitation bifurcation in the urban area of Beijing. -
The Use of Microwave Radiometer Data for Characterizing Snow Storage in Western China
Annals of Glaciology 16 1992 © International Glaciological Society The use of microwave radiometer data for characterizing snow storage in western China A. T. C. CHANG,]. L. FOSTER, D. K. HALL, Hydrological Sciences Branch, NASA Goddard Space Flight Center, Greenbelt, Maryland, U.S.A. D. A. ROBINSON, Department if Geography, Rutgers University, New Brullswick, New Jersey, U.S.A. LI PEIJI AND CAO MEISHENG Lanzhou Institute of Glaciology and Geocryology, Academia Sinica, Lanzhou 730000, China ABSTRACT. In this study a new microwave snow retrieval algorithm was developed to account for the effects of atmospheric emission on microwave radiation over high-elevation land areas. This resulted in improved estimates of snow-covered area in western China when compared with the meteorological station data and with snow maps derived from visible imagery from the Defense Meteorological Satellite Program satellite. Some improvement in snow-depth estimation was also achieved, but a useful level of accuracy will require additional modifications tested against more extensive ground data. INTRODUCTION In the present study an algorithm was developed to account for the effect of atmospheric constituents on In areas of high mountains, where snowmelt runoff makes microwave radiation emerging from a snowpack. This up a large portion of the water supply, snow-cover and resulted in improved snow-depth estimates when com snow-storage information are vital for management of pared with meteorological station data. water resources. ~ In western China, the varying snow extent and storage may influence the Asian summer monsoon and be linked to summer precipitation in MICROWAVE EMISSION FROM SNOW southeastern China (Barnett and others, 1989; Hahn and Shukla, 1976). -
Outcome Budget of the Department of Space Government of India 2013-2014 Contents
OUTCOME BUDGET OF THE DEPARTMENT OF SPACE GOVERNMENT OF INDIA 2013-2014 CONTENTS Page Nos. Executive Summary (i) - (ii) Introduction (Organisational Set-up, Major Projects/ Programmes of Department of Space, Overview Chapter I of 12th Five Year Plan 2012-2017 proposals, 1-13 Mandate and Policy framework of Department of Space) Chapter II Outcome Budget 2013-2014 15-60 Chapter III Reform measures and Policy initiatives 61-62 Review of Performance of the Major ongoing Chapter IV 63-102 Projects/Programmes/Centres of DOS/ISRO Chapter V Financial Review 103-110 Chapter VI Autonomous Bodies of DOS/ISRO 111-119 Annexure Major Indian Space Missions EXECUTIVE SUMMARY i. The primary objective of the Indian Space Programme is to achieve self-reliance in Space Technology and to evolve application programme to meet the developmental needs of the country. Towards meeting this objective, two major operational space systems have been established – the Indian National Satellite (INSAT) for telecommunication, television broadcasting and meteorological service and the Indian Remote Sensing Satellite (IRS) for natural resource monitoring and management. Two operational launch vehicles, Polar Satellite Launch Vehicle (PSLV) and Geosynchronous Satellite Launch Vehicle (GSLV) provide self reliance in launching IRS & INSAT Satellites respectively. ii. The Department of Space (DOS) and the Space Commission was set up in 1972 to formulate and implement Space policies and programmes in the country. The Indian Space Research Organisation (ISRO) is the research and development wing of the Department of Space and is responsible for executing the programmes and schemes of the Department in accordance with the directives and policies laid down by the Space Commission and the DOS. -
Instrument Intercomparison – Paul Simona 1 DRAGON ADVANCED TRAINING COURSE in ATMOSPHERE REMOTE SENSING Atmospheric Remote Sensing Measurements
DRAGON ADVANCED TRAINING COURSE IN ATMOSPHERE REMOTE SENSING 4. Satellite Validation Principle C o r r e l a t i v e D a t Day 4 Lecture 2 Instrument intercomparison – Paul Simona 1 DRAGON ADVANCED TRAINING COURSE IN ATMOSPHERE REMOTE SENSING Atmospheric Remote Sensing Measurements • Atmosphere is continuously changing in time and space. => No repeated measurements of the same quantity. • Radiation field measurements are direct, all other are indirect • Measurements probe large atmospheric volume => Large averaging and validation by in situ measurements difficult Courtesy Erkki Kyrola Day 4 Lecture 2 Instrument intercomparison – Paul Simon 2 DRAGON ADVANCED TRAINING COURSE IN ATMOSPHERE REMOTE SENSING Atmospheric Satellite Sensors We launch a satellite sensor for dedicated purposes: Meteorology, dynamical tracer, surface UV monitoring; Global climatology; Montreal and Kyoto Protocol related issues; Atmospheric processes: polar chemistry, etc.; Tropospheric issues like pollution, biomass burning, oxidizing capacity…; Radiative Transfer and Chemical Transport modelling. Day 4 Lecture 2 Instrument intercomparison – Paul Simon 3 DRAGON ADVANCED TRAINING COURSE IN ATMOSPHERE REMOTE SENSING Satellite Validation Principles Ideally, the observations of atmospheric constituents must not be dependent on: ¾ the atmospheric temperature; ¾ the abundance of other species; ¾ the Sun elevation; ¾ the presence of clouds; ¾ the instrument degradation (aging); ¾ etc… Day 4 Lecture 2 Instrument intercomparison – Paul Simon 4 DRAGON ADVANCED TRAINING -
Helsinki University of Technology
Aalto University School of Science Degree Programme in Industrial Engineering and Management Timo Tuomivirta Energy management in neighbourhoods Master’s Thesis Espoo, 07/06/2016 Supervisor: Professor Jan Holmström Instructor: M.Sc. Olli Nummelin Title of thesis Energy management in neighbourhoods Degree programme Industrial Engineering and Management Major Industrial Management Code of major TU-22 Supervisor Professor Jan Holmström Thesis advisor M.Sc. Jan Holmström Date 07.06.2016 Number of pages 115+67 Language English The topic of the thesis was to structure, refine, combine, analyse, and model data from real estate. Possibilities to adjust the relationship of utilities demand and supply were evaluated. The information collected from real estate was composed of real estate level and apartment level data. Real estate level data included weather, heating circuit, cooling circuit and domestic water. The apartment level data included room temperature switch, room operating panel and domestic hot-, and cold water consumption. The apartment specific data were aggregated on real estate level. First the interrelation of sub meters and utility companies billing were formed. After that the differences between measurements and company billing were evaluated. Then system specifically on certain time resolution the temperature of supply and return water, electricity consumption, heat energy consumption and cool energy consumption were determined. Hot water, cold water and overall water consumption on certain time resolution were determined. Furthermore, the seasonal ratio of hot and cold water was evaluated. From cold water station related data sample width specific energy efficiency ratio were calculated. From room temperature switch and room operating panel real estate level analysis were aggregated. -
Synthetic Aperture Radar (SAR) (L-Band, Res
University of Rome “Sapienza”, Faculty of Enginnering, Aula del Chiostro, June 14th, 2016 1 SPACE BASED RADAR: A SECRET START 21/12/1964: Quill (P-40), NRO experimental satellite of Corona Program. 1st SAR in orbit (all weather all time imaging) Due to the poor quality, images were considered useless and the program was discontinued (secret until 9 July 2012) RADAR ALTIMETRY: A NEW START IN 1973 14/5/1973 Skylab: mission included S-193, NASA & DoD experimental multimode instrument, including technology test of Radar Altimetry at 13,9 GHz. Positive results. 9/4/1975 Geodynamics Experimental Ocean Satellite (GEOS-3) : First satellite totally dedicated to radar altimetry (13,9 GHz, height accuracy=20 cm). Unexpected result: evaluation of surface wind speed from RA data 27/6/1978:Seasat, 3 out of 5 instruments were radar: Radar Altimeter: f.o. of GEOS-3, (Ku- band, accur. 10cm)Scatterometer and the “first official” Synthetic Aperture Radar (SAR) (L-band, Res. 25m) Quil Seasat 2 1981, 1984: SPACE SHUTTLE, A NEW OPPORTUNITY FOR EARTH OBSERVATION Apr. 12, 1981: Inaugural flight of the Space Shuttle. Nov. 12-14, 1981: OSTA-1,(Office of Space and Terrestrial Applications) comprised the first Shuttle Imaging Radar A (SIR-A). L band, resolution40x40 m, fixed look angle 47°, swath width 50 km, based on Seasat design, and using its spare parts as well as spare parts of other NASA missions (other 4 instruments were different passive sensors in VIS-IR) Oct. 5-13, 1984: OSTA-3, Shuttle Imaging Radar–B (SIR-B). Upgraded SIR-A, L band, resolution 30-20m (azimuth), 58-16m (range), variable look angle 15°-65°, swath width 50 km.