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Back to the the Future? 07> Probing the Kuiper Belt
SpaceFlight A British Interplanetary Society publication Volume 62 No.7 July 2020 £5.25 SPACE PLANES: back to the the future? 07> Probing the Kuiper Belt 634089 The man behind the ISS 770038 Remembering Dr Fred Singer 9 CONTENTS Features 16 Multiple stations pledge We look at a critical assessment of the way science is conducted at the International Space Station and finds it wanting. 18 The man behind the ISS 16 The Editor reflects on the life of recently Letter from the Editor deceased Jim Beggs, the NASA Administrator for whom the building of the ISS was his We are particularly pleased this supreme achievement. month to have two features which cover the spectrum of 22 Why don’t we just wing it? astronautical activities. Nick Spall Nick Spall FBIS examines the balance between gives us his critical assessment of winged lifting vehicles and semi-ballistic both winged and blunt-body re-entry vehicles for human space capsules, arguing that the former have been flight and Alan Stern reports on his grossly overlooked. research at the very edge of the 26 Parallels with Apollo 18 connected solar system – the Kuiper Belt. David Baker looks beyond the initial return to the We think of the internet and Moon by astronauts and examines the plan for a how it helps us communicate and sustained presence on the lunar surface. stay in touch, especially in these times of difficulty. But the fact that 28 Probing further in the Kuiper Belt in less than a lifetime we have Alan Stern provides another update on the gone from a tiny bleeping ball in pioneering work of New Horizons. -
Roll Calibration for Cryosat-2: a Comprehensive Approach
remote sensing Technical Note Roll Calibration for CryoSat-2: A Comprehensive Approach Albert Garcia-Mondéjar 1,* , Michele Scagliola 2 , Noel Gourmelen 3,4 , Jerome Bouffard 5 and Mònica Roca 1 1 isardSAT S.L., Barcelona Advanced Industry Park, 08042 Barcelona, Spain; [email protected] 2 Aresys SRL, 20132 Milano, Italy; [email protected] 3 School of GeoSciences, University of Edinburgh, Drummond Street, Edinburgh EH8 9XP, UK; [email protected] 4 IPGS UMR 7516, Université de Strasbourg, CNRS, 67000 Strasbourg, France 5 ESA ESRIN, 00044 Frascati, Italy; [email protected] * Correspondence: [email protected] Abstract: CryoSat-2 is the first satellite mission carrying a high pulse repetition frequency radar altimeter with interferometric capability on board. Across track interferometry allows the angle to the point of closest approach to be determined by combining echoes received by two antennas and knowledge of their orientation. Accurate information of the platform mispointing angles, in particular of the roll, is crucial to determine the angle of arrival in the across-track direction with sufficient accuracy. As a consequence, different methods were designed in the CryoSat-2 calibration plan in order to estimate interferometer performance along with the mission and to assess the roll’s contribution to the accuracy of the angle of arrival. In this paper, we present the comprehensive approach used in the CryoSat-2 Mission to calibrate the roll mispointing angle, combining analysis from external calibration of both man-made targets, i.e., transponder and natural targets. The roll calibration approach for CryoSat-2 is proven to guarantee that the interferometric measurements are exceeding the expected performance. -
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Research. Innovation. Sustainability PLANS FOR A NEW WAVE OF EUROPEAN SENTINEL SATELLITES The most ambitious and comprehensive plans ever for the European space sector, were approved at the end of 2019, with a total budget of ¤14.5 billion for the European Space Agency for the next three years – a 20% increase over the previous three-year budget. The decision allows a direct uplift to Europe’s Earth observation capability, expanding Copernicus – the European Union’s flagship Earth observation programme – with a suite of new, high-priority satellite missions. In this explainer we delve into the improvements and what they mean for sustainability and climate science. What is the Copernicus Programme? Copernicus is the European Union’s Earth observation programme, coordinated by the European Commission in partnership with the European Space Agency (ESA), EU Member States and other EU Agencies. Established in 2014, it builds on ESA’s Global Monitoring for Environment and Security (GMES) programme. Copernicus encompasses a system of satellites, airborne data, and ground stations supplying global monitoring data and operational services on a free-of-charge basis across six themes: atmosphere, marine, land, climate, emergency response and security. The Sentinel System – new and improved At the centre of the programme sits the Copernicus Space Component, which includes a family of satellites known collectively as Sentinels. These spacecraft provide routine atmospheric, oceanic, cryosphere and land global monitoring data, which are made freely available for Copernicus Services and major research and commercial applications such as precision farming, environmental hazards monitoring, weather forecasting and climate resilience. The soon-to-be-expanded Sentinel system will incorporate six high-priority missions. -
Sentinel-3 Product Notice
Copernicus S3 Product Notice – Altimetry Mission S3 Sensor SRAL / MWR Product LAND L2 NRT, STC and NTC Product Notice ID S3A.PN-STM-L2L.10 Issue/Rev Date 16/07/2020 Version 1.1 This Product Notice was prepared by the S3 Mission Performance Centre Preparation and ESA experts Approval ESA Mission Management Summary This is a Product Notice (PN) for the Copernicus Sentinel-3A and Sentinel-3B Surface Topography Mission (STM) Level-2 Land products at Near Real Time (NRT), Short Time Critical (STC) and Non Time Critical (NTC) timeliness. The Notice describes the STM current status, product quality and limitations, and product availability status. © ESA page 1 / 16 Processing Baseline S3A S3B Processing Baseline • Processing Baseline: 2.68 • Processing Baseline: 1.42 • • SR_1 IPF version: 06.18 SR_1 IPF version: 06.18 • MW_1 IPF version: 06.11 IPFs version • MW_1 IPF version: 06.11 • • SM_2 IPF version: 06.19 SM_2 IPF version: 06.19 Current Operational Processing Baseline IPF IPF Version In OPE since S3A SR1 06.18 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 S3A MW1 06.11 Land Centres: NRT mode : 2020-01-21 STC mode : 2020-01-21 NTC mode : 2020-01-21 S3A SM2 06.19 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 S3B SR1 06.18 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 S3B MW1 06.11 Land Centres: NRT mode : 2020-01-21 STC mode : 2020-01-21 NTC mode : 2020-01-21 S3B SM2 06.19 Land Centres: NRT mode : 2020-07-09 STC mode : 2020-07-09 NTC mode : 2020-07-09 © ESA page 2 / 16 Status of the Processing Baseline S3A The Processing Baseline (PB) for Copernicus Sentinel-3A STM products associated to this PN is reported above. -
About the Consistency Between Envisat and Cryosat-2 Radar Freeboard Retrieval Over Antarctic Sea Ice
The Cryosphere, 10, 1415–1425, 2016 www.the-cryosphere.net/10/1415/2016/ doi:10.5194/tc-10-1415-2016 © Author(s) 2016. CC Attribution 3.0 License. About the consistency between Envisat and CryoSat-2 radar freeboard retrieval over Antarctic sea ice Sandra Schwegmann1, Eero Rinne2, Robert Ricker1, Stefan Hendricks1, and Veit Helm1 1Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany 2Finnish Meteorological Institute, Marine Research, Erik Palménin aukio 1, 00560 Helsinki, Finland Correspondence to: Sandra Schwegmann ([email protected]) Received: 26 June 2015 – Published in The Cryosphere Discuss.: 16 September 2015 Revised: 6 June 2016 – Accepted: 8 June 2016 – Published: 8 July 2016 Abstract. Knowledge about Antarctic sea-ice volume and its 1 Introduction changes over the past decades has been sparse due to the lack of systematic sea-ice thickness measurements in this Over the last 3 decades, sea-ice extent (SIE) in the Arctic remote area. Recently, first attempts have been made to de- has decreased and submarine ice draft measurements indi- velop a sea-ice thickness product over the Southern Ocean cate that also sea-ice volume is declining (Rothrock et al., from space-borne radar altimetry and results look promising. 1999, 2008; Lindsay and Schweiger, 2015). In the Antarctic, Today, more than 20 years of radar altimeter data are poten- in contrast, SIE is increasing, but little is known about the tially available for such products. However, the characteris- changes in sea-ice volume. This is due to the lack of system- tics of individual radar types differ for the available altimeter atic sea-ice thickness measurements in the Southern Hemi- missions. -
Exploring the Benefits of Using Cryosat-2'S Cross-Track
JULY 2013 D I B A R B O U R E E T A L . 1511 Exploring the Benefits of Using CryoSat-2’s Cross-Track Interferometry to Improve the Resolution of Multisatellite Mesoscale Fields G. DIBARBOURE CLS, Ramonville St-Agne, France P. Y. LE TRAON IFREMER, Plouzane, France N. GALIN Centre for Polar Observation and Modelling, Department of Earth Sciences, University College London, London, United Kingdom (Manuscript received 7 August 2012, in final form 12 January 2013) ABSTRACT Sea surface height (SSH) measurements provided by pulse-limited radar altimeters are one-dimensional profiles along the satellite’s nadir track, with no information whatsoever in the cross-track direction. The anisotropy of resulting SSH profiles is the most limiting factor of mesoscale SSH maps that merge the 1D profiles. This paper explores the potential of the cross-track slope derived from the Cryosphere Satellite-2 (CryoSat- 2)’s synthetic aperture radar interferometry (SARin) mode to increase the resolution of mesoscale fields in the cross-track direction. Through idealized 1D simulations, this study shows that it is possible to exploit the dual SARin measurement (cross-track slope and SSH profile) in order to constrain mesoscale mapping in the cross-track direction. An error-free SSH slope allows a single SARin instrument to recover almost as much SSH variance as two coordinated altimeters. Noise-corrupted slopes can also be exploited to improve the mapping, and a break- through is observed for SARin errors ranging from 1 to 5 mrad for 150-km-radius features in strong currents, and 0.1–0.5 mrad for global mesoscale. -
Europe's Earth Observation, Satellite Navigation and Communications
Europe’s Earth Observation, Satellite Navigation and Communications Missions and Services for the benefit of the Arctic Inventory of current and future capabilities, their synergies and societal benefits Boniface, K., Gioia, C. Pozzoli, L., Diehl, T., Dobricic, S., Fortuny Guasch, J., Greidanus, H., Kliment, T., Kucera, J., Janssens- Maenhout, G., Soille, P., Strobl, P., and Wilson, J. 2021 EUR 30629 EN This publication is a Technical report by the Joint Research Centre (JRC), the European Commission’s science and knowledge service. It aims to provide evidence-based scientific support to the European policymaking process. The scientific output expressed does not imply a policy position of the European Commission. Neither the European Commission nor any person acting on behalf of the Commission is responsible for the use that might be made of this publication. For information on the methodology and quality underlying the data used in this publication for which the source is neither Eurostat nor other Commission services, users should contact the referenced source. The designations employed and the presentation of material on the maps do not imply the expression of any opinion whatsoever on the part of the European Union concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. Contact information Name: Karen Boniface Address: European Commission, Joint Research Centre, Directorate E: Space, Security and Migration Email: [email protected] Tel.: +39-0332-785295 EU Science Hub https://ec.europa.eu/jrc JRC121206 EUR 30629 EN PDF ISBN 978-92-76-32079-1 ISSN 1831-9424 doi:10.2760/270136 Luxembourg: Publications Office of the European Union, 2021 © European Union, 2021 The reuse policy of the European Commission is implemented by the Commission Decision 2011/833/EU of 12 December 2011 on the reuse of Commission documents (OJ L 330, 14.12.2011, p. -
ESA Propulsion Lab at ESTEC
ESA Propulsion Lab at ESTEC IEPC-2009-236 Presented at the 31st International Electric Propulsion Conference, University of Michigan • Ann Arbor, Michigan • USA September 20 – 24, 2009 J. Gonzalez del Amo*, G. Saccoccia† and P.-E. Frigot‡ European Space Agency, ESTEC, Keplerlaan 1, 2201 AG Noordwijk, The Netherlands Abstract: Electric and chemical propulsion systems are very important for spacecraft applications. Performance and reliability of propulsion systems are two main areas that have to be demonstrated to any space project. Europe is developing several types of electric and chemical thrusters for application to many satellites. Design, manufacturing and testing of such thrusters is a complex activity that requires a great effort. Full characterisation, qualification, acceptance and plume interaction tests are mandatory in the full assessment of these technologies. The ESA Propulsion Laboratory (EPL) is an operational facility at ESTEC in the spacecraft propulsion testing field. The EPL provides test services to the ESA Propulsion and Aerothermodynamics Division, which is responsible at European Space Agency for R&D activities and support to projects in the areas of chemical propulsion, electric and advanced propulsion and aerothermodynamics. When applicable, the EPL also provides technical advice and support to external organisations for subjects related to propulsion testing and test facilities. A laboratory dedicated to electric propulsion exists at ESTEC since early 1980s. In the last years, the activities of the laboratory, under project request, have been expanded to chemical propulsion (cold gas and other non-toxic propellants). During 2004, EPL has obtained dual ISO 17025 accreditation and ISO 9001 certification. In 2007 the EPL changed its physical location and several tests were performed in order to validate the correct functioning of the facilities This paper will describe the EPL organisation, facilities and activities after the physical relocation. -
Cryosat-2 for Inland Water Applications – Potential, Challenges and Future Prospects
Downloaded from orbit.dtu.dk on: Oct 08, 2021 CryoSat-2 for Inland Water Applications – Potential, Challenges and Future Prospects Kittel, Cecile Marie Margaretha; Jiang, Liguang; Schneider, R.; Andersen, Ole Baltazar; Nielsen, Karina; Bauer-Gottwein, Peter Published in: 25 years of progress in radar altimetry symposium - abstract book Publication date: 2018 Document Version Publisher's PDF, also known as Version of record Link back to DTU Orbit Citation (APA): Kittel, C. M. M., Jiang, L., Schneider, R., Andersen, O. B., Nielsen, K., & Bauer-Gottwein, P. (2018). CryoSat-2 for Inland Water Applications – Potential, Challenges and Future Prospects. In 25 years of progress in radar altimetry symposium - abstract book (pp. 85-85). European Space Agency. General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. Users may download and print one copy of any publication from the public portal for the purpose of private study or research. You may not further distribute the material or use it for any profit-making activity or commercial gain You may freely distribute the URL identifying the publication in the public portal If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. → 25 YEARS OF PROGRESS IN RADAR ALTIMETRY SYMPOSIUM © ESA 2018 ABSTRACT BOOK 24–29 September 2018 | Ponta Delgada, São Miguel Island Azores Archipelago, Portugal ABSTRACT BOOK 25 Years of Progress in Radar Altimetry Workshop 24-29 September 2018 Ponta Delgada Azores Last update: 19 October 2018 1 Table of Contents 2 Committees ............................................................................................................................................... -
Cryosat Baseline-C Ocean Product Handbook
esrin Largo Galileo Galilei, 1 Casella Postale 64 00044 Frascati, Italy T +39 06 9418 01 F +39 06 9418 0280 www.esa.int Version 4.1 5th December 2019 Baseline-C CryoSat Ocean Processor Ocean Product Handbook Prepared by F. Mertz, JP Dumont and S Urien (CLS) CryoSat Ocean Processor developers Approved by: J. Bouffard (ESA - ESRIN) CryoSat Data Quality Manager P. Féménias (ESA - ESRIN CryoSat ESA Technical Officer CryoSat Ocean Product Handbook V 4.1 i.1 Chronology Issues: Issue: Date: Reason for change: Author 1.0 26/04/13 Creation F. Mertz JP Dumont S Urien 2.0 10/06/13 Update for AR F. Mertz 3.0 27/10/17 Update for Cryosat-2 Ocean Processing Baseline C S Urien (CONFORM, SAMOSA, update of geophysical models) 4.0 05/12/17 ESA final review and update J. Bouffard 4.1 05/12/19 Update to account for POE-F orbit solution S. Urien Index Sheet: Context: Keywords: CryoSat, Satellite Altimetry, Ocean product, Baseline C Hyperlink: Distribution: Company Means of distribution Names CLS Notification J.P. Dumont S. Urien ACS Electronic Copy P.L. Mantovani ESA Electronic Copy J. Bouffard P. Féménias Applicable documents CryoSat Ocean Product Handbook V 4.1 i.2 AD 1 IPF Cryosat Ocean Products Contract Change Notice C2-CN-ACS-GS-5309 AD 2 Earth Explorer Ground Segment File Format Standard PE-TN-ESA-GS-0001 AD 3 IOP & GOP Product Format Specification Products format specification [COP-FMT], CS-RS-ACS-GS-5213 1rev4, https://earth.esa.int/documents/10174/125273/CryoSat-L1b-L2-Ocean- NetCDF-product-format-specification.pdf AD 4 CryoSat Ocean NetCDF Product Format Specification (L1b&L2) [PFS-OCE] CS-RS-ACS-ESL-5266 3rev1 AD 5 CryoSat Baseline D Product Handbook, 2019: https://earth.esa.int/documents/10174/125272/CryoSat-Baseline-D-Product- Handbook Reference documents RD 1 Bouffard, J., M. -
The European Space Agency's Earth Explorer Mission Cryosat
Annals of Glaciology 39 2004 313 The European Space Agency’s Earth Explorer Mission CryoSat: measuring variability in the cryosphere Mark R. DRINKWATER,1 Richard FRANCIS,1 Guy RATIER,1 Duncan J. WINGHAM2 1Earth Observation Programmes Directorate, European Space Agency, Postbus 299, 2200 AG Noordwijk, The Netherlands E-mail: [email protected] 2Centre for Polar Observation and Modelling, University College London, Gower Street, London WC1E 6BT, UK ABSTRACT. CryoSat is currently being prepared for a 2005 launch as the first European Space Agency Earth Explorer Opportunity mission. It is a dedicated cryospheric mission equipped with a Ku-band SIRAL (SAR/Interferometric Radar ALtimeter), whose primary objectives are to measure the variability and trends in the mass of the Arctic sea-ice cover and large terrestrial ice sheets. In this paper, an overview is provided of the mission and of the measurement characteristics of the new SIRAL instrument. Examples of data acquired on recent preparatory campaigns are presented, illustrating the operating characteristics of the key SIRAL modes. Preparatory plans for calibration and validation of CryoSat data are described. INTRODUCTION fluctuations and trends in the mass of the Earth’s major land- Variations in the mass of continental and sea-ice fields have and sea-ice fields, and to address the scientific issues implications for the rate of sea-level change, and the Earth’s described in the previous section. The natural variability in radiation budget and ocean thermohaline circulation, sea- and land-ice elevation observed by an altimeter is respectively. Until recently, the fluctuation in turnover of determined by changes in mass flux from the atmosphere continental ice mass was only known to an accuracy of and ocean, as well as changes in snow and ice density. -
Altimetry for the Future: Building on 25 Years of Progress
Available online at www.sciencedirect.com ScienceDirect Advances in Space Research xxx (xxxx) xxx www.elsevier.com/locate/asr Altimetry for the future: Building on 25 years of progress International Altimetry Teamà Received 16 August 2020; received in revised form 11 January 2021; accepted 13 January 2021 Abstract In 2018 we celebrated 25 years of development of radar altimetry, and the progress achieved by this methodology in the fields of glo- bal and coastal oceanography, hydrology, geodesy and cryospheric sciences. Many symbolic major events have celebrated these devel- opments, e.g., in Venice, Italy, the 15th (2006) and 20th (2012) years of progress and more recently, in 2018, in Ponta Delgada, Portugal, 25 Years of Progress in Radar Altimetry. On this latter occasion it was decided to collect contributions of scientists, engineers and man- agers involved in the worldwide altimetry community to depict the state of altimetry and propose recommendations for the altimetry of the future. This paper summarizes contributions and recommendations that were collected and provides guidance for future mission design, research activities, and sustainable operational radar altimetry data exploitation. Recommendations provided are fundamental for optimizing further scientific and operational advances of oceanographic observations by altimetry, including requirements for spatial and temporal resolution of altimetric measurements, their accuracy and continuity. There are also new challenges and new openings men- tioned in the paper that are particularly crucial for observations at higher latitudes, for coastal oceanography, for cryospheric studies and for hydrology. The paper starts with a general introduction followed by a section on Earth System Science including Ocean Dynamics, Sea Level, the Coastal Ocean, Hydrology, the Cryosphere and Polar Oceans and the ‘‘Green” Ocean, extending the frontier from biogeochemistry to marine ecology.