Satellite Altimetry. The range R from satellite to mean sea level is estimated by.

Slides:

Advertisements

Similar presentations

Phase change on Reflection, Refraction. S A B C N P E T AIR t i r r i r r L L M i Q O P r U U.

Advertisements

OUTLINE Motivation Modeling Simulation Experiments Conclusions.

The Telephone transmitter loudspeaker (Sound energy to electrical energy) (Electrical energy to sound energy)

Draft Recommendations subtitle here. Recommendation 1 The study groups from this workshop continue to collaborate with the goal of reporting progress.

26/11/2012 – Observatoire de Paris Analysis of wind speed evolution over ocean derived from altimeter missions and models M. Ablain (CLS)

Tracking an Atlantic Wave Storm with Jason-2 Altimeter Sérgio Muacho - IPMA.

7. Radar Meteorology References Battan (1973) Atlas (1989)

Calibration Scenarios for PICASSO-CENA J. A. REAGAN, X. WANG, H. FANG University of Arizona, ECE Dept., Bldg. 104, Tucson, AZ MARY T. OSBORN SAIC,

04 Feb 2008_rkraney COASTAL ALTIMETER WORKSHOP 1 The Delay-Doppler Altimeter R. K. Raney Briefing for the Coastal Altimetry Workshop Johns Hopkins University.

The Aquarius Salinity Retrieval Algorithm Frank J. Wentz and Thomas Meissner, Remote Sensing Systems Gary S. Lagerloef, Earth and Space Research David.

SAR Altimetry in Coastal Zone: Performances, Limits, Perspectives Salvatore Dinardo Serco/ESRIN Bruno Lucas Deimos/ESRIN Jerome Benveniste ESA/ESRIN.

Why is the sky blue? Why are clouds white? Why are sunsets red?

Radar Remote Sensing RADAR => RA dio D etection A nd R anging.

MR P.Durkee 5/20/2015 MR3522Winter 1999 MR Remote Sensing of the Atmosphere and Ocean - Winter 1999 Active Microwave Radar.

Distance observations

Spatial-Temporal Parametric Model with Covariance Structure based on Multiple Satellite Altimetry for Predicting and Interpolating Sea Surface Heights.

ASIC**3 Workshop -- May 2006 Measuring Global Sea Level Rise With Satellite Radar Altimetry ASIC**3 Workshop -- May 2006 Laury Miller NOAA/NESDIS Lab for.

3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process.

Surface Water and Ocean Topography Mission (SWOT)

Radar Many in a series of McGourty- Rideout Productions.

Satellite observation systems and reference systems (ae4-e01) Signal Propagation E. Schrama.

Naval Weapons Systems Energy Fundamentals Learning Objectives  Comprehend basic communication theory, electromagnetic (EM) wave theory  Comprehend.

A Prelude to HHT Analysis My work led to but before the HHT.

Uncertainty of sea level rise, rankings etc. First some results on the temperature hiatus.

Spaceborne Weather Radar

HY-2A Satellite Altimetric data Evaluation in the Arctic Ocean Yongcun Cheng Ole Baltazar Andersen.

R ADAR By: Abdullah Khan(09ES18). W HAT IS R ADAR ? RADAR (Radio Detection And Ranging) is a way to detect and study far off targets by transmitting a.

ODINAFRICA/GLOSS Sea Level Training Course

Chapter 7: Light Figure 7.8 Good APCs: 2, 3, 5, 6, 9, 10, 14, 18, 19, 20, 22, 23, 25, 28, 29, 30, 31, 42, 45, 46, and 48.

Sample Presentation Slides RADAR Operator Instruction.

Remote Sensing: Observing a BIG COUNTRY David Griffin & Edward King CSIRO Marine and Atmospheric Research.

OC3522Summer 2001 OC Remote Sensing of the Atmosphere and Ocean - Summer 2001 Active Microwave Radar.

Guided Notes on Gathering Weather Data

ESEOO meeting, Santiago de Compostela, january 2007 Improved satellite altimetry for the observation of shelf/coastal dynamics The Margins Altimetry Projects.

IRI Workshop 2005 TEC Measurements with Dual-Frequency Space Techniques and Comparisons with IRI T. Hobiger, H. Schuh Advanced Geodesy, Institute of Geodesy.

Sea Level Change Measurements: Estimates from Altimeters Understanding Sea Level Rise and Variability June 6-9, 2006 Paris, France R. S. Nerem, University.

June, 2003EUMETSAT GRAS SAF 2nd User Workshop. 2 The EPS/METOP Satellite.

GEOF334 – Spring 2010 Radar Altimetry Johnny A. Johannessen Nansen Environmental and Remote Sensing Center, Bergen, Norway.

Data management: Data sources & Quality control. Sea level measurements.

Philip Moore Jiasong Wang School of Civil Engineering and Geosciences University of Newcastle upon Tyne Newcastle upon Tyne NE1 7RU

PiLDo Labs CryoSat Workshop, 9/2/ SIRAL Beam-formation Verification using Transponders Mònica Roca and Mercedes Reche PiLDo Labs, Barcelona.

Gathering Weather Data pg. 79. Surface Data Instruments thermometer- filled with mercury or alcohol; expands when heated barometer- measures air pressure;

Sea ice thickness from CryoSat – A new data set for operational ice services? Christian Haas German CryoSat Office AWI.

Synthetic Aperture Radar at The Alaska SAR Facility

1 SVY 207: Lecture 12 GPS Error Sources: Part 2 –Satellite: ephemeris, clock, S/A, and A/S –Propagation: ionosphere, troposphere, multipath –Receiver:antenna,

OSTST - March Hobart 1 Impacts of atmospheric attenuations on AltiKa expected performances J.D. Desjonquères (1), N. Steunou (1) A. Quesney (2)

ELECTRONIC COMMUNICATIONS A SYSTEMS APPROACH CHAPTER Copyright © 2014 by Pearson Education, Inc. All Rights Reserved Electronic Communications: A Systems.

1 Satellite geodesy (ge-2112) Applications E. Schrama.

AMSR-E Vapor and Cloud Validation Atmospheric Water Vapor –In Situ Data Radiosondes –Calibration differences between different radiosonde manufactures.

Satellite Microwave Radiometry: Current and Future Products Rogre De Roo and Tony England Atmospheric, Oceanic, and Space Sciences.

GPS Radio-Occultation data (COSMIC mission) Lidia Cucurull NOAA Joint Center for Satellite Data Assimilation.

1 July 20, 2000 Geosat Follow-On An examination from an operational point of view Impact on operational products Overall system performance (from sensor.

SCM x330 Ocean Discovery through Technology Area F GE.

WP120 External Calibration of Spaceborne Microwave Remote Sensing System Sensors Objective:Evaluation of external calibration needs for a variety of microwave.

Signal Propagation Basics

Altimeter and scatterometer seminar SMHI, March 2012 Future of satellite altimeters Sentinel-3 and SWOT Julia Figa Saldaña With contributions from Sentinel-3.

ESA Climate Change Initiative Sea-level-CCI project A.Cazenave (Science Leader), G.Larnicol /Y.Faugere(Project Leader), M.Ablain (EO) MARCDAT-III meeting.

Active Microwave Remote Sensing

(2) Norut, Tromsø, Norway Improved measurement of sea surface velocity from synthetic aperture radar Morten Wergeland Hansen.

Visit for more Learning Resources

EGU2007-A-10154, NP6.04 Tuesday 17 of April, Vienna 2007

Signal Propagation Basics

Anomalous Propagation

GEOGRAPHIC INFORMATION SYSTEMS & RS INTERVIEW QUESTIONS ANSWERS

HMA-FO Task 1 EOP Metadata

The Telephone transmitter loudspeaker (Sound energy to

Weather Forecasting.

Propagation Effects on Communication Links

Coastal Altimetry Challenges

Atmospheric reanalysis at ECMWF

Presentation transcript:

Satellite Altimetry

The range R from satellite to mean sea level is estimated by

Past Missions

Current Missions

Radar Measurement principles

Normalized radar Cross Section

Ocean Surface Reflectivity

Atmospheric Attenuation Clear Sky Transmittance at normal incidence angle

Cloud Attenuation

Rain Attenuation

Two-Way Travel Time Pulse-Limited

Average Returned Waveform

Fig 16: Average of 1, 25, and 1000 Simulated Independent time series of illuminated area

Instrument Corrections Doppler Shift Altimeter Acceleration Error Oscillator Drift Error Pointing angle and sea-state correction

Foot Print Size

Range Estimation 1cm accuracy from satellite altimetry by measuring two-way travel time is a big challenge due to the reasons: Atmospheric Effects: Dry Tropospheric Refraction Wet Tropospheric Refraction Ionospheric Refraction Sea-State Effects: Electromagnetic Bias Skewness Bias

TECU estimated from Dual-freq measurements

Orbit Determination