Methods to improve Real-Time Visualization and Exploration of Precipitation and Temperature in Web-Cartography ICC 2009, Santiago de Chile Christophe Lienert,

Slides:



Advertisements
Similar presentations
List of Nominations Connecting User Needs with Weather Research and Forecasts Rebecca E. Morss National Center for Atmospheric Research Boulder, Colorado,
Advertisements

African Centre for Statistics United Nations Economic Commission for Africa Role of GIS and Remote Sensing to Environment Statistics Dozie Ezigbalike Data.
ICC 2009, Santiago de Chile Visualization of Glacier Surface Movement Samuel Wiesmann Institute of Cartography, ETH Zurich.
Climate changes in Southern Africa; downscaling future (IPCC) projections Olivier Crespo Thanks to M. Tadross Climate Systems Analysis Group University.
OBJECTIVES Evaporation, precipitation and atmospheric heating ‘communicate’ SSTA to the atmosphere, driving changes in temperature, precipitation and.
OBSERVATIONAL NETWORKS OPERATED BY THE NATIONAL OBSERVATORY OF ATHENS V.. Kotroni - K. Lagouvardos Institute of Environmental Research National Observatory.
WFM 6202: Remote Sensing and GIS in Water Management © Dr. Akm Saiful IslamDr. Akm Saiful Islam WFM 6202: Remote Sensing and GIS in Water Management Akm.
The Influence of Basin Size on Effective Flash Flood Guidance
Elsa Nickl and Cort Willmott Department of Geography
Raster Based GIS Analysis
ASTER image – one of the fastest changing places in the U.S. Where??
Harlan Shannon Meteorologist U.S. Department of Agriculture Office of the Chief Economist World Agricultural Outlook Board Washington D.C., U.S.A. An Overview.
Natural Hazards. Integrated Risk Assessment & Scientific Advice Uncertainty in forecasting and risk assessment Hydro-meteorologicalVolcanoesEarthquakes.
PROVIDING DISTRIBUTED FORECASTS OF PRECIPITATION USING A STATISTICAL NOWCAST SCHEME Neil I. Fox and Chris K. Wikle University of Missouri- Columbia.
Raster Data. The Raster Data Model The Raster Data Model is used to model spatial phenomena that vary continuously over a surface and that do not have.
Chapter 1 Ways of Seeing. Ways of Seeing the Atmosphere The behavior of the atmosphere is very complex. Different ways of displaying the characteristics.
1 Modelled Meteorology - Applicability to Well-test Flaring Assessments Environment and Energy Division Alex Schutte Science & Community Environmental.
Alan F. Hamlet Dennis P. Lettenmaier Center for Science in the Earth System Climate Impacts Group and Department of Civil and Environmental Engineering.
Signal, Instruments and Systems Project 5: Sensor accuracy in environmental sensor networks.
Climate Variability and Prediction in the Little Colorado River Basin Matt Switanek 1 1 Department of Hydrology and Water Resources University of Arizona.
Extreme Value Analysis, August 15-19, Bayesian analysis of extremes in hydrology A powerful tool for knowledge integration and uncertainties assessment.
Understanding Drought
A Very spatial Presentation. ANCIENT BABYLONIAN CLAY TABLETS DEPICT THE EARTH AS A FLAT CIRCULAR DISK EARLIEST DIRECT EVIDENCE OF MAPPING COMES FROM THE.
Kening Wang, Charles Stegman, Sean W. Mulvenon, and Yanling Xia University of Arkansas, Fayetteville, AR, Using Kriging and Interactive Graphics.
CARPE DIEM Centre for Water Resources Research NUID-UCD Contribution to Area-3 Dusseldorf meeting 26th to 28th May 2003.
Cyber-Infrastructure for Agro-Threats Steve Goddard Computer Science & Engineering University of Nebraska-Lincoln.
WP7 Adaptation to Climate Change in Latvia: Challenges for Society and Researchers Kristīne Āboliņa The University of Latvia Faculty of Geography and Earth.
Grid-based Analysis in GIS
Map Scale, Resolution and Data Models. Components of a GIS Map Maps can be displayed at various scales –Scale - the relationship between the size of features.
Application of GI-based Procedures for Soil Moisture Mapping and Crop Vegetation Status Monitoring in Romania Dr. Adriana MARICA, Dr. Gheorghe STANCALIE,
SERVIR-AFRICA: an overview André Kooiman International workshop on higher resolution Land cover mapping for the African continent UNEP, 27 June 2013.
Swedish Meteorological and Hydrological Institute SE Norrköping, SWEDEN COMPARISON OF AREAL PRECIPITATION ESTIMATES: A CASE STUDY FOR A CENTRAL.
ELDAS activities at SMHI/Rossby Centre – 2nd Progress Meeting L. Phil Graham Daniel Michelson Jonas Olsson Åsa Granström Swedish Meteorological and Hydrological.
BY:- RAVI MALKAT HARSH JAIN JATIN ARORA CIVIL -2 ND YEAR.
Name, Surname, Position Logo(s) Weather monitoring and forecasting over eastern Attica (Greece) in the frame of FLIRE project Vassiliki Kotroni (1), Konstantinos.
Seasonal hydrological forecasting from snow cover maps and climatological data using support vector machine M. Callegari, L. De Gregorio, P. Mazzoli, C.
Introduction to ArcGIS for Environmental Scientists Module 2 – Fundamentals Chapter 7 – Queries.
Application of a rule-based system for flash flood forecasting taking into account climate change scenarios in the Llobregat basin EGU 2012, Vienna Session.
GIS in Weather and Society Olga Wilhelmi Institute for the Study of Society and Environment National Center for Atmospheric Research.
Forecasting Streamflow with the UW Hydrometeorological Forecast System Ed Maurer Department of Atmospheric Sciences, University of Washington Pacific Northwest.
Downscaling and its limitation on climate change impact assessments Sepo Hachigonta University of Cape Town South Africa “Building Food Security in the.
Earth System Models NASA TOPS -- Terrestrial Observation and Prediction System (predictive capabilities of over 30 variables describing land surface conditions.
Advanced GIS Using ESRI ArcGIS 9.3 3D Analyst part 2.
Overview of the Colorado Basin River Forecast Center Lisa Holts.
RESULTS OF RESEARCH RELATED TO CHARIS IN KAZAKHSTAN I. Severskiy, L. Kogutenko.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Federal Departement of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Revisiting Swiss temperature trends * Paulo.
CARPE DIEM 6 th meeting – Helsinki Critical Assessment of available Radar Precipitation Estimation techniques and Development of Innovative approaches.
Renata Gonçalves Tedeschi Alice Marlene Grimm Universidade Federal do Paraná, Curitiba, Paraná 1. OBJECTIVES 1)To asses the influence of ENSO on the frequency.
Verification of Precipitation Areas Beth Ebert Bureau of Meteorology Research Centre Melbourne, Australia
Mapping Geographical Volumes: The Isarithmic Map SP 240 Cartography Alex Chaucer.
INTEGRATING SATELLITE AND MONITORING DATA TO RETROSPECTIVELY ESTIMATE MONTHLY PM 2.5 CONCENTRATIONS IN THE EASTERN U.S. Christopher J. Paciorek 1 and Yang.
1 Principles of symbolization Attribution (by) Licensees may copy, distribute, display and perform the work and make derivative works based on it only.
Enabling Climate Impact Assessment in Wisconsin Chris Kucharik and Dan Vimont The Wisconsin Initiative on Climate Change Impacts (WICCI)
NOAA Northeast Regional Climate Center Dr. Lee Tryhorn NOAA Climate Literacy Workshop April 2010 NOAA Northeast Regional Climate.
Applied Cartography and Introduction to GIS GEOG 2017 EL Lecture-5 Chapters 9 and 10.
Lecture 24: Uncertainty and Geovisualization
Spatial Models – Raster Stacy Bogan
Precipitation Classification and Analysis from AMSU
An Agriculture Perspective
Overview of Downscaling
Reinhold Steinacker Department of Meteorology and Geophysics
An Introduction to VegDRI
UW Civil and Environmental Engineering
Statistical surfaces: DEM’s
Road Weather Information Systems (RWIS)
Computer Vision Lecture 4: Color
Winter storm forecast at 1-12 h range
Chapter 2 Human Information Processing
Spatial interpolation
Presentation transcript:

Methods to improve Real-Time Visualization and Exploration of Precipitation and Temperature in Web-Cartography ICC 2009, Santiago de Chile Christophe Lienert, ETH Zurich

Overview  Motivation  User needs and objectives  Methodology – automated workflows for P and T  Map results  Discussion and Conclusion

Motivation > a changing climate  More intense, frequent precipitation and flood events  Statistically show: very rare events become rare events  Precipitation sees a seasonal shift from summer to winter  Shift of the 0°C line > decisive for flooding in spring / autumn

Motivation > damage reduction  Improve preparedness before floods, enhance monitoring  More assets and values lie in flood-prone areas  Increase of risks and damages (2005: 3 Mia CHF)

User Needs & Objectives RADAR TEMPERATURE DISTRIBUTION EXTRACTION OF 0°C ISOTHERM TEMPERATURE POINT GAUGES INTERSECTION - Visual enhancements - Show attributes - toggle views BETTER ASSESSMENTS of catchment‘s disposition to flooding Real-time generation

Precipitation Radar and Temperature Interpolation  Radar today > integrated, multi-parameter, quantitative  Difficulties: instrumental, meterological factors affect accuracy  main advantage: spatial extent of prec. fields clearly visible  Temperature data > often inavailable in higher altitudes  Difficulties: interpolation accuracy in mountainous topography 1h data ≠ 1day data  spatial variability depends on temporal variability  main advantage: altitude is the main distribution factor

Precipitation radar maps > existing examples  Radar > from stand-alone in the 1960s to user-oriented quantitative monitoring products, storm-tracking, now-casting  Radar > uncertainties due to instrumental and meteorological factors  Radar > main advantage: spatial extent of precipitation field  Temperature > accuracy of interpolation depending on observation accuracy, point density and  Discussion and Conclusion No quantitative color scheme Too many classes Too coarse Way too many classes

Visual Improvements Radar  Radar > continuous, quantitative data [mm] or [in]  Reduce number of data classes  Use sequential color scheme, vary lightness  Apply visual smoothing for more genuine representations

Temperature maps > existing examples No legend, no clear allocation No areal interpolation

Visual Improvements Temperature  Temperature > continuous quantitative data [°C] or [°K]  Use diverging color schemes  Contrast hue, vary lightness for + and - values  Use point symbolizations AND interpolated surfaces AND extracted isolines

Taking advantages of web-mapping  …to avoid representational conflicts radar vs. temperature  Web-maps > Data exploration with interactive methods!  Web-maps > central calculations, visualizations on the client

Methodology > real time workflow radar

Methodology > real time workflow temperature

Interpolated temperature surface - Display of legend on mouseover - Display of ommited gauges

Temperature surface + framed rectangles - Display of time series, attributes on click - Red and blue rectangles on gauge sites

Interactive, radar image - re-classifed, re-colored, bilinear smoothing - Legend directly displayed in ‚raster‘ tab

smoothed radar image + 0°C isotherm -highlighting of area above 0°C - attributes directly displayed in ‚vector‘ tab

Framed rectangles for point temperature data - tooltip function on mouseover - attributes and legends directly displayed in ‚vector‘ tab

Discussion  Visual problems:  Complex workflows  exception handling  Other ways of handling missing/faulty data?  Data problems:  Other interpolation methods?  Calculation of real-time environmental lapse rate?  Inclusion of longitudinal lapse rate? Solar radiance?

Conclusion  Visual Improvements of real time radar possible in real-time! (inappropriate class numbers, illegible coloring, coarse resolution data)  Visual improvements of point temperature data (framed rectangles)  Real-time interpolation of temperature points (iso-line and statistical surface)  Distribution of maps over the web (Combined views, interactive exploration methods, remote assessment)

Thank you for your attention! Christophe Lienert, ETH Zurich,