NASA Earth Science Senior Review 2015
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The Contribution of Global Ocean Observation of Continuity of HY-2
CGMS-XXXVI-CNSA-WP-04 Prepared by CNSA Agenda Item: III/3&4 The contribution of global ocean observation of continuity of HY-2 satellite HY-2 satellite, an ocean dynamic environment observation satellite, mainly ` objective is monitoring and detecting the parameters of ocean dynamic environment. These parameters include sea surface wind fields, sea surface height, wave height, gravity field, ocean circulation and sea surface temperature etc. The contribution of global ocean observation of continuity of HY-2 satellite 1. Introduction HY-2 satellite scatterometer provides sea surface wind fields, which can offset the observation gap of the plan of global scatterometer. At the same time, HY-2 satellite altimeter provides sea surface height, significant wave height, sea surface wind speed and polar ice sheet elevation, which can offset the observation gap of the plan of global altimeter around 2012, and can offset the observation gap of JASON-1&2 at polar area. More details as follows. 2. Observation of sea surface wind fields The analysis accuracy of wind field for ocean-atmosphere can improve 10-20% by using the satellite scatterometer data, by which can improve greatly the quality of initial wind field of numerical atmospheric forecast model in coastal ocean. Satellite scatterometer data has play important role on study of large-scale ocean phenomenon, such as sea-air interactions, ocean circulation, EI Nino etc. The figure 1 shows that QuikSCAT scatterometer has operational application in 1999, but it has not the following plan. ERS-2 scatterometer mission has transferred to METOP ASCAT in 2006. GCOM-B1 will launch in 2008, one of its payloads is an ocean vector wind measurement (OVWM) instruments, and it also called AlphaScat. -
Unmanned Aerial System Nadir Reflectance and MODIS Nadir BRDF
The Cryosphere, 11, 1575–1589, 2017 https://doi.org/10.5194/tc-11-1575-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Unmanned aerial system nadir reflectance and MODIS nadir BRDF-adjusted surface reflectances intercompared over Greenland John Faulkner Burkhart1,2, Arve Kylling3, Crystal B. Schaaf4, Zhuosen Wang5,6, Wiley Bogren7, Rune Storvold8, Stian Solbø8, Christina A. Pedersen9, and Sebastian Gerland9 1Department of Geosciences, University of Oslo, Oslo, Norway 2University of California, Merced, CA, USA 3Norwegian Institute for Air Research, Kjeller, Norway 4School for the Environment, University of Massachusetts Boston, Boston, MA, USA 5NASA Goddard Space Flight Center, Greenbelt, MD, USA 6Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA 7U.S. Geological Survey, Flagstaff, AZ, USA 8Norut-Northern Research Institute, Tromsø, Norway 9Norwegian Polar Institute, Fram Centre, Tromsø, Norway Correspondence to: John Faulkner Burkhart ([email protected]) Received: 12 November 2016 – Discussion started: 15 December 2016 Revised: 17 May 2017 – Accepted: 18 May 2017 – Published: 4 July 2017 Abstract. Albedo is a fundamental parameter in earth sci- data demonstrate potentially large sub-pixel variability of ences, and many analyses utilize the Moderate Resolu- MODIS reflectance products and the potential to explore this tion Imaging Spectroradiometer (MODIS) bidirectional re- variability using the UAS as a platform. It is also found that, flectance distribution function (BRDF)/albedo (MCD43) al- even at the low elevations flown typically by a UAS, re- gorithms. While derivative albedo products have been eval- flectance measurements may be influenced by haze if present uated over Greenland, we present a novel, direct compar- at and/or below the flight altitude of the UAS. -
In Brief Modified to Increase Engine Reliability
r bulletin 102 — may 2000 3rd Space Station ESA, together with a European industrial Element to be Launched consortium headed by DaimlerChrysler (D) and including Belgian, Dutch and French NASA and the Russian Aviation and partners, was responsible for the design, Space Agency (Rosaviakosmos) plan that development and delivery of the core data the next component of the International management system, which provides Space Station (ISS) – the Zvezda service Zvezda’s main computer. module – will be launched on 12 July from the Baikonur Cosmodrome in Kazakhstan. ESA also has a contract with Rosaviakosmos and RSC-Energia for Following a Joint Programme Review and performing system and interface a General Designers’ Review in Moscow, it integration tasks required for docking with was agreed that Zvezda (Russian for Zvezda by ESA’s Automated Transfer ‘star’) will be launched by a Proton rocket Vehicle (ATV), which will be used for ISS with the second and third stage engines re-boost and logistics support missions In Brief modified to increase engine reliability. from 2003 onwards. Through its ATV industrial consortium led by Aerospatiale Zvezda will provide the early living quarters Matra Lanceurs (F), ESA is also procuring for ISS crew, together with the life sup- some Russian hardware and software for port, electrical power distribution, data use with the ATV. management, flight control, and propul- sion systems for the ISS. On the scientific side, ESA has concluded contracts with Rosaviakosmos and RSC- Energia for the conduct of scientific experiments on Zvezda, including the Global Timing System (GTS) and a radiobiology experiment (called Matroshka) to monitor and analyse radiation doses in ISS crew. -
Estimating Gale to Hurricane Force Winds Using the Satellite Altimeter
VOLUME 28 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY APRIL 2011 Estimating Gale to Hurricane Force Winds Using the Satellite Altimeter YVES QUILFEN Space Oceanography Laboratory, IFREMER, Plouzane´, France DOUG VANDEMARK Ocean Process Analysis Laboratory, University of New Hampshire, Durham, New Hampshire BERTRAND CHAPRON Space Oceanography Laboratory, IFREMER, Plouzane´, France HUI FENG Ocean Process Analysis Laboratory, University of New Hampshire, Durham, New Hampshire JOE SIENKIEWICZ Ocean Prediction Center, NCEP/NOAA, Camp Springs, Maryland (Manuscript received 21 September 2010, in final form 29 November 2010) ABSTRACT A new model is provided for estimating maritime near-surface wind speeds (U10) from satellite altimeter backscatter data during high wind conditions. The model is built using coincident satellite scatterometer and altimeter observations obtained from QuikSCAT and Jason satellite orbit crossovers in 2008 and 2009. The new wind measurements are linear with inverse radar backscatter levels, a result close to the earlier altimeter high wind speed model of Young (1993). By design, the model only applies for wind speeds above 18 m s21. Above this level, standard altimeter wind speed algorithms are not reliable and typically underestimate the true value. Simple rules for applying the new model to the present-day suite of satellite altimeters (Jason-1, Jason-2, and Envisat RA-2) are provided, with a key objective being provision of enhanced data for near-real- time forecast and warning applications surrounding gale to hurricane force wind events. Model limitations and strengths are discussed and highlight the valuable 5-km spatial resolution sea state and wind speed al- timeter information that can complement other data sources included in forecast guidance and air–sea in- teraction studies. -
Let Me Just Add That While the Piece in Newsweek Is Extremely Annoying
From: Michael Oppenheimer To: Eric Steig; Stephen H Schneider Cc: Gabi Hegerl; Mark B Boslough; [email protected]; Thomas Crowley; Dr. Krishna AchutaRao; Myles Allen; Natalia Andronova; Tim C Atkinson; Rick Anthes; Caspar Ammann; David C. Bader; Tim Barnett; Eric Barron; Graham" "Bench; Pat Berge; George Boer; Celine J. W. Bonfils; James A." "Bono; James Boyle; Ray Bradley; Robin Bravender; Keith Briffa; Wolfgang Brueggemann; Lisa Butler; Ken Caldeira; Peter Caldwell; Dan Cayan; Peter U. Clark; Amy Clement; Nancy Cole; William Collins; Tina Conrad; Curtis Covey; birte dar; Davies Trevor Prof; Jay Davis; Tomas Diaz De La Rubia; Andrew Dessler; Michael" "Dettinger; Phil Duffy; Paul J." "Ehlenbach; Kerry Emanuel; James Estes; Veronika" "Eyring; David Fahey; Chris Field; Peter Foukal; Melissa Free; Julio Friedmann; Bill Fulkerson; Inez Fung; Jeff Garberson; PETER GENT; Nathan Gillett; peter gleckler; Bill Goldstein; Hal Graboske; Tom Guilderson; Leopold Haimberger; Alex Hall; James Hansen; harvey; Klaus Hasselmann; Susan Joy Hassol; Isaac Held; Bob Hirschfeld; Jeremy Hobbs; Dr. Elisabeth A. Holland; Greg Holland; Brian Hoskins; mhughes; James Hurrell; Ken Jackson; c jakob; Gardar Johannesson; Philip D. Jones; Helen Kang; Thomas R Karl; David Karoly; Jeffrey Kiehl; Steve Klein; Knutti Reto; John Lanzante; [email protected]; Ron Lehman; John lewis; Steven A. "Lloyd (GSFC-610.2)[R S INFORMATION SYSTEMS INC]"; Jane Long; Janice Lough; mann; [email protected]; Linda Mearns; carl mears; Jerry Meehl; Jerry Melillo; George Miller; Norman Miller; Art Mirin; John FB" "Mitchell; Phil Mote; Neville Nicholls; Gerald R. North; Astrid E.J. Ogilvie; Stephanie Ohshita; Tim Osborn; Stu" "Ostro; j palutikof; Joyce Penner; Thomas C Peterson; Tom Phillips; David Pierce; [email protected]; V. -
Remote Sensing (Test)
Scioly Summer Study Session 2017 Remote Sensing (Test) Topic: Climate Change Pro c esses* ___ By user whythelongface (merge) Name(s): _________________________________________ Test format: This test is worth 150 points. There are four sections: 1. Remote Sensing Technology and techniques (50 points) ___ /50 2. Data Use and Manipulation (20 points) ___ /20 3. Image Interpretation (30 points) ___ /30 4. Weather and Climate Processes (50 points) ___ /50 Total: ___ /150 As of the 2016-2017 season, each person is allowed one double-sided 8.5 × 11” notesheet. Each partnership is allowed a protractor, ruler, writing implements, and a scientific calculator. Graphing calculators are not allowed. The author wishes you best of luck on this test and in the 2017-2018 Science Olympiad season. *The topic for the 2017-2018 season is still unknown at the time this test is being written, so it will focus on the same topic as that of the 2016-2017 season. Part 1: Remote Sensing Technology Multiple Choice (1 point each) -
Diurnal Variation of Stratospheric Hocl, Clo and HO2 at the Equator
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Atmos. Chem. Phys. Discuss., 12, 21065–21104, 2012 Atmospheric www.atmos-chem-phys-discuss.net/12/21065/2012/ Chemistry doi:10.5194/acpd-12-21065-2012 and Physics © Author(s) 2012. CC Attribution 3.0 License. Discussions This discussion paper is/has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP if available. Diurnal variation of stratospheric HOCl, ClO and HO2 at the equator: comparison of 1-D model calculations with measurements of satellite instruments M. Khosravi1, P. Baron2, J. Urban1, L. Froidevaux3, A. I. Jonsson4, Y. Kasai2,5, K. Kuribayashi2,5, C. Mitsuda6, D. P. Murtagh1, H. Sagawa2, M. L. Santee3, T. O. Sato2,5, M. Shiotani7, M. Suzuki8, T. von Clarmann9, K. A. Walker4, and S. Wang3 1Department of Earth and Space Sciences, Chalmers University of Technology, Gothenburg, Sweden 2National Institute of Information and Communications Technology, Tokyo, Japan 3Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA 4Tokyo Institute of Technology, Kanagawa, Japan 5Tokyo Institute of Technology, Yokohama, Japan 6Fujitsu FIP Corporation, Tokyo, Japan 7Research Institute for Sustainable Humanosphere, Kyoto University, Kyoto, Japan 8Japan Aerospace Exploration Agency, Ibaraki, Japan 21065 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | 9Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany Received: 10 May 2012 – Accepted: 20 July 2012 – Published: 20 August 2012 Correspondence to: M. Khosravi ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 21066 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract The diurnal variation of HOCl and the related species ClO, HO2 and HCl mea- sured by satellites has been compared with the results of a one-dimensional pho- tochemical model. -
A Report on the Way Forward Based on the Review of Research Gaps and Priorities
A Report on the Way Forward Based on the Review of Research Gaps and Priorities Sponsored by the Environmental Working Group of the U.S. NextGen Joint Planning and Development Office Lead Coordinating Author Dr. Guy P. Brasseur NCAR This report can be accessed via the internet at the following FAA website http://www.faa.gov/about/office_org/headquarters_offices/aep/aviation_climate/ 1 Table of Contents Preface.……………………………………………………………………………………………5 Executive Summary..……………………………………………………………………………...7 Chapter 1…………………………………………………………………………………………12 Introduction Chapter 2…………………………………………………………………………………............17 Contrails and Induced Cirrus: Microphysics and Climate Impact Chapter 3…………………………………………………………………………………………24 Contrails and Induced Cirrus: Optics and Radiation Chapter 4…………………………………………………………………………………………28 Chemistry and Transport Processes in the Upper Troposphere and Lower Stratosphere Chapter 5…………………………………………………………………………………………35 Climate Impacts Metrics for Aviation Chapter 6…………………………………………………………………………………………40 The Way Forward References………………………………………………………………………………………..43 Appendix I: List of ACCRI Subject Specific Whitepapers…………………………………...49 Appendix II: ACCRI Science Meeting Agenda………………………………………………..50 Appendix III: List of ACCRI Science Meeting Participants……………………………………53 2 Author Team* Preface Authors: Mohan Gupta and Lourdes Maurice, FAA; Cindy Newberg, EPA; Malcolm Ko, John Murray and Jose Rodriguez, NASA; David Fahey, NOAA Executive Summary Author: Guy Brasseur, NCAR Chapter I Introduction Author: Guy Brasseur, NCAR -
Improved Quality Control for Quikscat Near Real-Time Data
JP4.6 Improved Quality Control for QuikSCAT Near Real-time Data S. Mark Leidner, Ross N. Hoffman, and Mark C. Cerniglia Atmospheric and Environmental Research Inc., Lexington, Massachusetts Abstract errors. We will illustrate the types of errors that occur due to rain contamination and ambiguity removal. SeaWinds on QuikSCAT, launched in June 1999, We will also give examples of how the quality of the provides a new source of surface wind information retrieved winds varies across the satellite track, and over the world’s oceans. This new window on global varies with wind speed. surface vector winds has been a great aid to real- SeaWinds is an active, Ku-band microwave radar time operational users, especially in remote areas operating near ¢¤£¦¥¨§ © and is sensitive to centimeter- of the world. As with in situ observations, the qual- scale or capillary waves on the ocean surface. ity of remotely-sensed geophysical data is closely These waves are usually in equilibrium with the wind. tied to the characteristics of the instrument. But Each radar backscatter observation samples a patch remotely-sensed scatterometer winds also have a of ocean about . The vector wind is re- whole range of additional quality control concerns trieved by combining several backscatter observa- different from those of in situ observation systems. tions made from multiple viewing geometries as the The retrieval of geophysical information from the raw scatterometer passes overhead. The resolution of satellite measurements introduces uncertainties but the retrieved winds is . also produces diagnostics about the reliability of the Backscatter from capillary waves on the ocean retrieved quantities. -
Earth Science Data and Information System (ESDIS) Project Update
Earth Science Data and Information System (ESDIS) Project Update October 15-16, 2008 National Snow and Ice Data Center & Physical Oceanography DAAC User Working Group Meeting Pasadena, CA [email protected] ESDIS Project Code 423 NASA GSFC Topics •• ESDISESDIS OrganizationOrganization •• SystemSystem ContextContext •• KeyKey MetricsMetrics •• DataData ArchitectureArchitecture •• KeyKey ActivitiesActivities – Data Discovery – Customer Satisfaction & Metrics – Operations Management 2 Earth Science Data and Information System (ESDIS) Project • The ESDIS Project is responsible for the Earth Observing System Data and Information System (EOSDIS), one of the largest civilian Science Information System in the world • The EOSDIS: – Ingests, archives, processes, and distributes an unprecedented volume of science data for NASA’s flagship Earth science missions (e.g., Terra, Aqua, Aura, ICESat) – Supports unique requirements of a variety of Earth science disciplines (e.g., land, atmosphere, snow/ice, and ocean) as well as inter- disciplinary researchers, climate This Jason sea-surface height image shows modelers, and application users sea surface height anomalies with the seasonal cycle (the effects of summer, fall, (e.g., U.S. Forest Service) winter, and spring) removed. Each image is a 10-day average of data, centered on the date – Employs state-of-the-art hardware indicated. and software technology to achieve Courtesy: NASA EOSDIS Physical 3 Oceanography DAAC required data throughput EOSDIS Manages Data For All 24 EOS Measurements Aqua (5/02) -
Highlights in Space 2010
International Astronautical Federation Committee on Space Research International Institute of Space Law 94 bis, Avenue de Suffren c/o CNES 94 bis, Avenue de Suffren UNITED NATIONS 75015 Paris, France 2 place Maurice Quentin 75015 Paris, France Tel: +33 1 45 67 42 60 Fax: +33 1 42 73 21 20 Tel. + 33 1 44 76 75 10 E-mail: : [email protected] E-mail: [email protected] Fax. + 33 1 44 76 74 37 URL: www.iislweb.com OFFICE FOR OUTER SPACE AFFAIRS URL: www.iafastro.com E-mail: [email protected] URL : http://cosparhq.cnes.fr Highlights in Space 2010 Prepared in cooperation with the International Astronautical Federation, the Committee on Space Research and the International Institute of Space Law The United Nations Office for Outer Space Affairs is responsible for promoting international cooperation in the peaceful uses of outer space and assisting developing countries in using space science and technology. United Nations Office for Outer Space Affairs P. O. Box 500, 1400 Vienna, Austria Tel: (+43-1) 26060-4950 Fax: (+43-1) 26060-5830 E-mail: [email protected] URL: www.unoosa.org United Nations publication Printed in Austria USD 15 Sales No. E.11.I.3 ISBN 978-92-1-101236-1 ST/SPACE/57 *1180239* V.11-80239—January 2011—775 UNITED NATIONS OFFICE FOR OUTER SPACE AFFAIRS UNITED NATIONS OFFICE AT VIENNA Highlights in Space 2010 Prepared in cooperation with the International Astronautical Federation, the Committee on Space Research and the International Institute of Space Law Progress in space science, technology and applications, international cooperation and space law UNITED NATIONS New York, 2011 UniTEd NationS PUblication Sales no. -
Cloudsat CALIPSO
www.nasa.gov andSpaceAdministration National Aeronautics & CloudSat CALIPSO Clean air is important to everyone’s health and well-being. Clean air is vital to life on Earth. An average adult breathes more than 3000 gallons of air every day. In some places, the air we breathe is polluted. Human activities such as driving cars and trucks, burning coal and oil, and manufacturing chemicals release gases and small particles known as aerosols into the atmosphere. Natural processes such as for- est fires and wind-blown desert dust also produce large amounts of aerosols, but roughly half of the to- tal aerosols worldwide results from human activities. Aerosol particles are so small they can remain sus- pended in the air for days or weeks. Smaller aerosols can be breathed into the lungs. In high enough con- centrations, pollution aerosols can threaten human health. Aerosols can also impact our environment. Aerosols reflect sunlight back to space, cooling the Earth’s surface and some types of aerosols also absorb sunlight—heating the atmosphere. Because clouds form on aerosol particles, changes in aerosols can change clouds and even precipitation. These effects can change atmospheric circulation patterns, and, over time, even the Earth’s climate. The Air We Breathe The Air We We need better information, on a global scale from satellites, on where aerosols are produced and where they go. Aerosols can be carried through the atmosphere-traveling hundreds or thousands of miles from their sources. We need this satellite infor- mation to improve daily forecasts of air quality and long-term forecasts of climate change.