Release Notes for Version 7 of the WegenerNet Processing System (WPS Level-2 data v7)

Similar documents
The WegenerNet observing weather and climate at 1 km-scale resolution: a new look at convective precipitation and other local-scale processes

WegenerNet: A new climate station network in Eastern Styria/Austria for monitoring weather and climate at 1 km-scale resolution

WegenerNet climate station network region Feldbach, Engineering Austria: network structure, processing system, example results

Verification of Operational Analyses Using an Extremely High-Density Surface Station Network

WeatherHawk Weather Station Protocol

Gridding of precipitation and air temperature observations in Belgium. Michel Journée Royal Meteorological Institute of Belgium (RMI)

2.12 Inter-Comparison of Real-Time Rain Gage and Radar-Estimated Rainfall on a Monthly Basis for Midwestern United States Counties

UWM Field Station meteorological data

4.5 Comparison of weather data from the Remote Automated Weather Station network and the North American Regional Reanalysis

Added Value of Convection Resolving Climate Simulations (CRCS)

MxVision WeatherSentry Web Services Content Guide

Data Quality Assurance System. Hong Kong, China

The Australian Operational Daily Rain Gauge Analysis

Studying Topography, Orographic Rainfall, and Ecosystems (STORE)

Non-Acoustical Inputs

PRODUCT USER MANUAL For GLOBAL Ocean Waves Analysis and Forecasting Product GLOBAL_ANALYSIS_FORECAST_WAV_001_027

Combining Deterministic and Probabilistic Methods to Produce Gridded Climatologies

Open Source ENKI: Dynamic Environmental Model Framework. A possible pre-processor for WRF-Hydro?

Description of the case study

Web GIS Based Disaster Portal Project ESRI INDIA

Model Output Statistics (MOS)

Speedwell High Resolution WRF Forecasts. Application

A TEST OF THE PRECIPITATION AMOUNT AND INTENSITY MEASUREMENTS WITH THE OTT PLUVIO

8-km Historical Datasets for FPA

Applications. Remote Weather Station with Telephone Communications. Tripod Tower Weather Station with 4-20 ma Outputs

USING GRIDDED MOS TECHNIQUES TO DERIVE SNOWFALL CLIMATOLOGIES

Basins-Level Heavy Rainfall and Flood Analyses

Climate Information for Managing Risk. Victor Murphy NWS Southern Region Climate Service Program Mgr. June 12, 2008

Wind Resource Assessment Practical Guidance for Developing A Successful Wind Project

Module 11: Meteorology Topic 3 Content: Weather Instruments Notes

PLANNED UPGRADE OF NIWA S HIGH INTENSITY RAINFALL DESIGN SYSTEM (HIRDS)

YOPP archive: needs of the verification community

Analysis of meteorological measurements made over three rainy seasons in Sinazongwe District, Zambia.

MesoWest: One Approach to Integrate Surface Mesonets

Aurora Bell*, Alan Seed, Ross Bunn, Bureau of Meteorology, Melbourne, Australia

Climate Prediction Center National Centers for Environmental Prediction

an experiment to assess the hydrological value of a portable X-band radar

Austrian Wind Atlas and Wind Potential Analysis

Memo. I. Executive Summary. II. ALERT Data Source. III. General System-Wide Reporting Summary. Date: January 26, 2009 To: From: Subject:

Measuring solid precipitation using heated tipping bucket gauges: an overview of performance and recommendations from WMO SPICE

Appendix 4 Weather. Weather Providers

Progress in Operational Quantitative Precipitation Estimation in the Czech Republic

The WOLF system: forecasting wet-snow loads on power lines in Italy

Quick Start Guide New Mountain Visit our Website to Register Your Copy (weatherview32.com)

REQUIREMENTS FOR WEATHER RADAR DATA. Review of the current and likely future hydrological requirements for Weather Radar data

Southern Heavy rain and floods of 8-10 March 2016 by Richard H. Grumm National Weather Service State College, PA 16803

Development of procedures for calibration of meteorological sensors. Case study: calibration of a tipping-bucket rain gauge and data-logger set

A Century of Meteorological Observations at Fort Valley Experimental Forest: A Cooperative Observer Program Success Story

WindNinja Tutorial 3: Point Initialization

The Global Precipitation Climatology Centre (GPCC) Serving the Hydro-Climatology Community

Application of Probability Density Function - Optimal Interpolation in Hourly Gauge-Satellite Merged Precipitation Analysis over China

McArthur River Mining Borroloola Caravan and Devils Spring Stations

A sensitivity and uncertainty analysis. Ministry of the Walloon Region Agricultural Research Centre

ERAD Challenges for precipitation estimation in mountainous regions. Proceedings of ERAD (2002): c Copernicus GmbH 2002

Prediction of Snow Water Equivalent in the Snake River Basin

QPE and QPF in the Bureau of Meteorology

CHAPTER 1 INTRODUCTION

J17.3 Impact Assessment on Local Meteorology due to the Land Use Changes During Urban Development in Seoul

Application and verification of ECMWF products in Norway 2008

Comparative analysis of data collected by installed automated meteorological stations and manual data in Central Asia.

Evaluating extreme flood characteristics of small mountainous basins of the Black Sea coastal area, Northern Caucasus

WMO SPICE. World Meteorological Organization. Solid Precipitation Intercomparison Experiment - Overall results and recommendations

Regional influence on road slipperiness during winter precipitation events. Marie Eriksson and Sven Lindqvist

Evaluation of MPE Radar Estimation Using a High Density Rain Gauge Network within a Hydro-Estimator Pixel and Small SubWatershed

Deliverable: D3.6. Description of the. final version of all gridded data sets of the climatology of the Carpathian Region

DETECTION AND FORECASTING - THE CZECH EXPERIENCE

Application and verification of ECMWF products 2008

Better Decisions for Your Business Drive your company forward with ultra-precise weather forecasts

4 Precipitation. 4.1 Rainfall characteristics

URBAN HEAT ISLAND IN SEOUL

Data Short description Parameters to be used for analysis SYNOP. Surface observations by ships, oil rigs and moored buoys

Austrian Wind Potential Analysis - AuWiPot

Using the EartH2Observe data portal to analyse drought indicators. Lesson 4: Using Python Notebook to access and process data

Sea ice charts and SAR for sea ice classification. Patrick Eriksson Juha Karvonen Jouni Vainio

Flood Forecasting Tools for Ungauged Streams in Alberta: Status and Lessons from the Flood of 2013

IMPACT OF GROUND-BASED GPS PRECIPITABLE WATER VAPOR AND COSMIC GPS REFRACTIVITY PROFILE ON HURRICANE DEAN FORECAST. (a) (b) (c)

AN INTERNATIONAL SOLAR IRRADIANCE DATA INGEST SYSTEM FOR FORECASTING SOLAR POWER AND AGRICULTURAL CROP YIELDS

Intercomparision of snowfall measured by weighing and tipping bucket precipitation gauges at Jumla Airport, Nepal

Data recovery and rescue at FMI

WindNinja Tutorial 3: Point Initialization

The retrieval of the atmospheric humidity parameters from NOAA/AMSU data for winter season.

Climate Data for Non-experts: Standards-based Interoperability

QualiMET 2.0. The new Quality Control System of Deutscher Wetterdienst

Some details about the theoretical background of CarpatClim DanubeClim gridded databases and their practical consequences

Tutorial 10 - PMP Estimation

FireFamilyPlus Version 5.0

The Impact of Horizontal Resolution and Ensemble Size on Probabilistic Forecasts of Precipitation by the ECMWF EPS

Application and verification of the ECMWF products Report 2007

Surface Hydrology Research Group Università degli Studi di Cagliari

Supplementary Materials for

WM9280. Pro Family weather station with T/H sensor, pluviometer, anemometer, PC connection and Meteotime weather forecasts until 3 days

An Evaluation of Seeding Effectiveness in the Central Colorado Mountains River Basins Weather Modification Program

New Intensity-Frequency- Duration (IFD) Design Rainfalls Estimates

A Comparison of Rainfall Estimation Techniques

Finnish Open Data Portal for Meteorological Data

SOUTH MOUNTAIN WEATHER STATION: REPORT FOR QUARTER 2 (APRIL JUNE) 2011

Presented at WaPUG Spring Meeting 1 st May 2001

1 Introduction. Station Type No. Synoptic/GTS 17 Principal 172 Ordinary 546 Precipitation

Product Description. 1 of 6

Guidelines on Quality Control Procedures for Data from Automatic Weather Stations

Transcription:

Release Notes for Version 7 of the WegenerNet Processing System (WPS Level-2 data v7) WegenerNet Tech. Report No. 1/2018 J. Fuchsberger, G. Kirchengast, and T. Kabas March 2018 Wegener Center for Climate and Global Change, University of Graz, Austria

Contents 1 Version Details 5 2 Major Changes 7 2.1 Level-2 Data Quality Indicators........................ 7 2.1.1 Station Time Series Data....................... 7 2.1.2 Gridded Data.............................. 9 2.2 NetCDF files.................................. 13 2.2.1 NetCDF version............................ 13 2.2.2 Coordinates............................... 13 3 New Features and Products 15 3.1 Level-1 data processing Quality Control System (QCS)......... 15 3.1.1 Wind spike check............................ 15 3.1.2 Relative humidity problem detection................. 15 3.1.3 1-minute data.............................. 16 3.2 Level-2 data processing Data Product Generator (DPG)........ 16 3.2.1 Homogenization of temperature and humidity data......... 16 3.2.2 Correction of precipitation data.................... 17 3.2.3 Johnsbachtal Level-2 data processing................. 17 3.2.4 High-resolution gridded wind fields.................. 17 3.3 Data portal................................... 17 3.3.1 Image export of plots......................... 17 3.3.2 Digital elevation model and land use/land cover data download.. 18 Bibliography 19 3

1 Version Details This document describes major changes and new features for version 7.9 of the WegenerNet Processing System (WPS), producing Level-1 data version 5 and Level-2 data version 7. WPS Version: 7.9 released March 22, 2018 Level-1 Data Version: 5 Level-2 Data Version: 7 (used to assign the general name of the version: WPS v7) 5

2 Major Changes 2.1 Level-2 Data Quality Indicators 2.1.1 Station Time Series Data Basis Data In common with previous versions of the WPS, data quality for Level-2 basis data is indicated by a Data Product Flag (DP-Flag) ranging from 0 to 4 (Table 2.1). Measurements that have passed the Level-1 Quality Control procedure with a Quality-Flag (Q-Flag) of 0 get a DP-Flag of 0, all other data are either temporally or spatially interpolated (Kirchengast et al. 2014, Ebner 2017). Level-2 basis data have a temporal resolution of 5 minutes for the WegenerNet Feldbach Region (FBR), and 10 minutes for the WegenerNet Johnsbachtal (JBT). Table 2.1: Data Product Flags for Level-2 basis data and corresponding properties (adapted from Ebner 2017, p. 9). DP-Flag Property of parameter value 0 Measured value at station that has passed Level-1 Quality Control 1 Temporally interpolated value 2 Spatially interpolated value (by surrounding stations) 3 Spatially interpolated value (by gridded data) 4 NaN value (no interpolation possible due to lack of data) Weather and Climate Data For Weather and Climate data, the DP-Flag s approach and meaning has changed: Instead of a value between 0 and 4 it now gets a percentage value between 0 % and 100 % which represents the flagged percentage of data (FP-of-Data), FP. FP is defined as a) for continuous data, like temperature and humidity: FP c = N[DP-Flag > 0] N total 100 [%], (2.1) 7

2 Major Changes where N[DP-Flag > 0] is the number of flagged basis data values, and N total is the total number of basis data values within the given timespan of a weather or climate data product. So, for example, if half of the temperature values of a given hour (N total = 12) are flagged, the resulting FP for this hour would be 6 12 = 50 %. For the given day (N total = 288), if only this single half hour was flagged, FP would be 6 288 = 1 48 = 2.1 %; b) for precipitation data: FP P = P flagged [mm] P total [mm] 100 [%], (2.2) where P flagged is the precipitation sum over all flagged basis data values, and P total is the total precipitation sum for a given timespan (T ) of a weather or climate data product, N T P flagged = {P i DP-Flag(P i ) > 0}, (2.3) i=1 N T P total = P i, (2.4) i=1 where index i runs over the timespan T up to final value N T. In order to ensure that only wet data (data with a reasonable minimum precipitation) are flagged, FP P is set to zero if the flagged precipitation sum is 0, or the maximum precipitation is below a certain low limit, i.e., if P flagged 0 or max(p i ) < 0.21 mm then FP P = 0; (2.5) For instance, if the precipitation sum of a given hour is 2 mm and half of this sum (1 mm) originates from flagged data, FP P for this hour would be 50 %. If the precipitation sum for the given day would be 4 mm, and the flagged data remains the same (1 mm), FP P for this day would be exactly 25 % ( 1 4 ), regardless of the timespan of the flagged precipitation data. This way of computation guarantees that precipitation flags are always properly weighted to the amount of precipitation. 8

2.1 Level-2 Data Quality Indicators 2.1.2 Gridded Data Basis Data As of WPS v7, gridded DP-Flag fields are generated out of the station s DP-Flags, serving as spatially resolved quality indicators. The DP-Flags of the individual stations are interpolated onto the grid using the same algorithm as used for the corresponding measurement values (inverse-distance weighted interpolation for temperature and humidity, and inverse-distance-squared interpolation for precipitation data). Fig. 2.1 shows two examples of DP-Flag fields for precipitation data, one on Aug. 27, 2017, 18:50-18:55 UTC (upper panel), the other on Feb. 13, 2018, 16:55-17:00 UTC (lower panel). On 27th Aug. 2017, all but two stations got a DP-Flag of 0 so that the respective DP-Flag field is essentially zero everywhere except for the two locations. On 13th Feb. 2018, as the temperature was below 2 C at all stations (the implemented criteria to distinguish between liquid and solid precipitation), only stations with heated precipitation gauges got a DP-Flag of 0. All other data have been spatially interpolated from the surrounding heated stations and thus got a DP-Flag of 2. Weather and Climate Data Weather and Climate data quality grids likewise use the flagged percentage of data (FPof-Data), FP, as described in section 2.1.1. However, instead of a calculation per station, FP is now calculated per grid point. The same equations (Eq. 2.1 to 2.4) are used for this purpose, just with the threshold DP-Flag > 0.5 instead of DP-Flag > 0 in Eqs. 2.1 and 2.3 now, in order to allow moderate deviations from zero for these interpolated grid point DP-Flag values. In order to make sure on the grid that only wet data (data with a reasonable minimum precipitation) are flagged, FP P is set to zero if the areal mean precipitation is below a certain low limit, i.e., if P total (x, y) < 0.21 mm then FP P = 0, (2.6) where P total (x, y) denotes the average precipitation over all grid points (x, y). Fig. 2.2 shows two examples of daily FP-of-Data fields for precipitation, one for 27th Aug. 2017 (upper panel) and the other for 12th Feb. 2018 (lower panel). Since on 27th Aug. 2017 the majority of stations had a FP-of-Data at or close to zero, the daily field also shows very low FP-of-Data over almost the entire region. On 12th Feb. 2018, as the temperature was below 2 C at most stations, only the heated ones have a FP-of-Data of 0. All other data have a percentage of 100 %, except a few stations where temperature exceeded 2 C for a short period. Fig. 2.3 shows the corresponding precipitation data for both examples. 9

2 Major Changes Figure 2.1: Gridded DP-Flag data for precipitation on 2017-08-27 18:50-18:55 UTC (upper panel) and on 2018-02-12 16:55-17:00 UTC (lower panel). 10

2.1 Level-2 Data Quality Indicators Figure 2.2: Map of flagged percentage (FP) of data for daily precipitation on 2017-08-27 (upper panel) and on 2018-02-12 (lower panel). 11

2 Major Changes Figure 2.3: Daily precipitation data for 2017-08-27 (upper panel) and for 2018-02-12 (lower panel). 12

2.2 NetCDF files 2.2 NetCDF files 2.2.1 NetCDF version The netcdf (Unidata, 2018) format version for all gridded data changed from 3.0 (classic) to 4.4. Version 4 NetCDF data are encoded using new compression options which led to a reduction in storage size by about a factor of four. 2.2.2 Coordinates UTM coordinates and projection information are now written directly into the netcdf files, making it easier to import them into GIS programs. Nevertheless, latitude/longitude coordinates are still available in a separate file for convenience, downloadable at https: //wegenernet.org/downloads/wn_l2_grid_v2_utm.nc. 13

3 New Features and Products 3.1 Level-1 data processing Quality Control System (QCS) 3.1.1 Wind spike check Because some wind sensors show unrealistic wind speed spikes (Fig. 3.1 illustrates an example), an additional QCS check has been implemented in QCS layer 4 (time variability checks), for generating the Level-1 data as basis for the WPS v7 Level-2 data. This so called wind spike check looks for anomalous spikes in the wind speed or gust data and compares their magnitude to the median and standard deviation of the data before the spike occurred. It is defined that any wind speed or gust value v s,i is flagged if v s,i > F m median(v j ) v s,i > F s stddev(v j ), (3.1) where v s is the spike magnitude, v j the wind speed or peak gust values of the last 120 minutes (24 data values), and F m, F s are constant coverage factors, depending on the parameter type and status of the sensor as summarized in Table 3.1. Table 3.1: Values for coverage factors F m and F s of the wind spike check. Parameter Sensor status F m F s Wind speed Normal 4.3 5.5 Wind speed Problem 2.5 4.5 Peak gust Normal 6.0 6.0 Peak gust Problem 2.5 4.5 See Scheidl (2014) and Scheidl et al. (2017) for further details on the QCS. 3.1.2 Relative humidity problem detection Since the first generation of relative humidity sensors in the WegenerNet are known to suffer from problems above humidity values of about 70 %RH, an elaborated special algorithm has been developed to detect problematic behavior and mark those values with a quality flag. The algorithm has been implemented into the QCS for the Level-1 data version 5 processing. Details can be found in Scheidl et al. (2017). 15

3 New Features and Products Figure 3.1: Wind speed data from station 501 with false-data spikes marked in red. 3.1.3 1-minute data As all 13 main stations in the FBR network have been recently changed to a native resolution of 1-minute, done while installing a new generation of data loggers, the QCS has been adapted for also processing these higher-resolved Level-1 data. However, for continuity and consistency reasons, the data are aggregated to 5-minutes in the Level-2 processing. For access to the Level-1 1-minute data, expert users can manually choose the Level-1 Version 5 data in the data selection dialog of the WegenerNet web portal. 3.2 Level-2 data processing Data Product Generator (DPG) 3.2.1 Homogenization of temperature and humidity data Temperature and humidity data have been homogenized according to Ebner (2017). The correction factors reported in this study were applied in Level-2 basis data processing of WPS v7. They therefore automatically apply also to the derived weather and climate data. 16

3.3 Data portal 3.2.2 Correction of precipitation data Implementation of correction curve for Meteoservis MR3 sensors Current precipitation sensors in the WegenerNet, Meteoservis MR3 and MR3H (Wegener Center, 2018) came shipped with a correction curve (METEOSERVIS, 2008), which can be used for compensation of undercatchment at high rain rates, typical for tipping-bucket sensors. The correction curve is applied during Level-2 basis data processing of WPS v7. For example, the network s record rain rate (by March 22, 2018) was observed on July 8, 2015, 13:25-13:30 UTC at station 11 with a rain rate of 20.1 mm/5 min ( 241 mm/h). Without correction, this event would be observed at 17.3 mm/5 min ( 208 mm/h). Implementation of correction factors for Friedrichs and Young sensors General correction factors of 1.10 for Friedrichs and 1.13 for Young sensors, operational from year 2007 until fall 2016 in the FBR network, have been implemented into the Level-2 processing of WPS v7 according to O et al. (2018). 3.2.3 Johnsbachtal Level-2 data processing As of Level-2 version 7, station time series data for the WegenerNet JBT network are also available as basis data and weather and climate data products. Due to the mountainous topography and the sparser station density (11 JBT stations in comparison to the 154 FBR stations by March 22, 2018), gridded data products for the main parameters temperature, relative humidity, and precipitation are not available for the JBT. 3.2.4 High-resolution gridded wind fields High-resolution wind fields and peak gust fields with a temporal resolution of 30 minutes and a spatial resolution of 100 m 100 m are generated every hour for both regions, the FBR and JBT, in the Level-2 processing of WPS v7. Also the complete FBR data record since 2007 and the JBT data since 2012 have been re-processed to produce these fields. As the other Level-2 data, the wind fields are aggregated to weather and climate data products. For details on data preparation see Schlager et al. (2017) and Schlager et al. (2018). 3.3 Data portal 3.3.1 Image export of plots As a new feature, all plots generated at the data portal can be exported as png images using the button Export plots as.png images at the bottom of the screen. 17

3 New Features and Products 3.3.2 Digital elevation model and land use/land cover data download In the grid data download section, digital elevation data in 10 m 10 m, 100 m 100 m, and 200 m 200 m resolution, covering the FBR and JBT regions (Land Steiermark, 2018), and land use/land cover data in 100 m 100 m resolution, covering the Styrian Raab catchment and WegenerNet FBR region (Klebinder et al., 2017), are now available for download. 18

Bibliography Ebner, S. (2017). Analysis and Homogenization of WegenerNet Temperature and Humidity Data and Quality Evaluation for Climate Trend Studies. Scientific Report No.70-2017, ISBN 978-3-9503918-9-3, Wegener Center Verlag, Graz, Austria. (pdf, 7.6 MB). Kirchengast, G., Kabas, T., Leuprecht, A., Bichler, C., and Truhetz, H. (2014). WegenerNet A pioneering high-resolution network for monitoring weather and climate. Bull. Amer. Meteor. Soc., 95:227 242. doi:10.1175/bams-d-11-00161.1 (pdf, 2.5 MB). Klebinder, K., Sotier, B., Lechner, V., and Strauss, P. (2017). Hydrologische und hydropedologische Kenndaten Raabgebiet und Region Südoststeiermark. Technical report, Department of Natural Hazards, Austrian Research Center for Forests (BFW), Innsbruck, Austria. (pdf, 4.7 MB). Land Steiermark (2018). GIS-Steiermark. http://www.gis.steiermark.at. Land Steiermark, Amt der Steiermärkischen Landesregierung, Graz, Austria. Accessed 22nd March 2018. METEOSERVIS (2008). Correction curve for mr3, mr3h. (pdf, 0.3 MB). O, S., Foelsche, U., Kirchengast, G., and Fuchsberger, J. (2018). Validation and correction of rainfall data from the WegenerNet high density network in southeast Austria. J. Hydrol., 556:1110 1122. doi:10.1016/j.jhydrol.2016.11.049. Scheidl, D. (2014). Improved quality control for the WegenerNet and demonstration for selected weather and climate events. Scientific Report No.61-2014, ISBN 978-3- 9503608-8-2, Wegener Center Verlag, Graz, Austria. (pdf, 3.3 MB). Scheidl, D., Fuchsberger, J., and Kirchengast, G. (2017). Analysis of the quality of WegenerNet humidity data and improvements. Scientific Report No.74-2017, ISBN 978-3-9504501-2-5, Wegener Center Verlag, Graz, Austria. (pdf, 4.6 MB). Schlager, C., Kirchengast, G., and Fuchsberger, J. (2017). Generation of high-resolution wind fields from the WegenerNet dense meteorological station network in southeastern Austria. Wea. Forecast., 32(4):1301 1319. doi:10.1175/waf-d-16-0169.1. Schlager, C., Kirchengast, G., and Fuchsberger, J. (2018). Empirical high-resolution wind field and gust model in mountainous and hilly terrain based on the dense wegenernet station networks. Atmos. Meas. Tech., submitted manuscript. 19

BIBLIOGRAPHY Unidata (2018). Network common data form (netcdf) version 4.4.1.1 [software]. Boulder, CO: UCAR/Unidata. doi:10.5065/d6h70cw6. Wegener Center (2018). Wegenernet data fact sheet version 14. (pdf, 0.5 MB). Accessed 22nd March 2018. 20