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This study compares the precipitation verification of four different COSMO models at 7 km resolution (COSMO-I7, COSMO-7, COSMO-EU, COSMO-ME) with two models at 2 km resolution (COSMO-I2, COSMO-IT). The dataset consists of high-resolution rain gauge data from the COSMO dataset and Civil Protection Department. The study aims to analyze seasonal trends and the performance of each model version.
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Precipitation verification comparison among COSMO-I7, COSMO-EU, COSMO-7, COSMO-ME, COSMO-I2, COSMO-IT (Elena Oberto, Massimo Milelli - ARPA Piemonte) • QPF verification of the 4 model versions at 7 km res. (COSMO-I7, COSMO-7, COSMO-EU, COSMO-ME) with the 2 model versions at 2 km res. (COSMO-I2, COSMO-IT) • Specifications: • Dataset: high resolution network of rain gauges coming from COSMO dataset and Civil Protection Department 1300 stations • Method: 24h/6h averaged cumulated precipitation value over 90 meteo-hydrological basins • The aims: • Long period verification (seasonal trend) • Verification ovest last year (200706-200806)
Verification over last year (200706-200806) COSMO-7/COSMO-EU • Not so strong differences • COSMO-7 sligtly better on average
Verification over last year (200706-200806) COSMO-7/COSMO-EU • Strong differences during the single season • COSMO-EU quite stable overestimation • COSMO-7 bias and pod decrease (far reduction)
Verification over last year (200706-200806) COSMO-I7/COSMO-ME • Not so strong differences • COSMO-ME sligtly better on average
Verification over last year (200706-200806) COSMO-I7/COSMO-ME • Strong differences during the single season • COSMO-ME quite stable overestimation • COSMO-I7 bias and pod decrease
Verification over last year (200706-200806) COSMO-I7/COSMO-I2 • COSMO-I2 sligtly better on average
Verification over last year (200706-200806) COSMO-I7/COSMO-I2 • COSMO-I2 trend seems to follow COSMO-I7 trend • COSMO-I2 worsening: strong positive bias last summer (deep convection on), negative bias this spring (deep convection off)
Verification over last year (200706-200806) COSMO-ME/COSMO-IT • No significant differences
Verification over last year (200706-200806) COSMO-ME/COSMO-IT • Generally the same trend • bias > 1 • Sligltly improvement for pod, ets,far
Verification over last year (200706-200806) Diurnal cycle • Bias overestimation peak during midday • Best value peak for pod, ets, far during afternoon • Spin-up problem for all the models especially COSMO-I7 and COSMO-I2
Verification over last year (200706-200806) Diurnal cycle • General worsening with forecast time • The spin-up seems to disappear except for COSMO-I2 • Anomalous behaviour for COSMO-I2 • COSMO-7 underestimates
Summarizing… • Trend over long period: general slight improvement with the exception of COSMO-7 and COSMO-I7 for the last seasons • Intercomparison model verification over 200706-200806: • COSMO-EU and COSMO-ME quite stable overestimation • COSMO-7 bias and pod decrease • COSMO-I7 bias and pod decrease • COSMO-I2 worsening: strong bias >1 last summer (deep convection on), bias < 1 this spring (deep convection off) • Similar performance for COSMO-ME and COSMO-IT • 3. Diurnal cycle over 200706-200806: • Bias overestimation peak during midday • Best values of pod, ets, far during afternoon • Spin-up problem for low thresholds • General worsening with the forecast time • General overestimation with the exception of COSMO-7
COSMO-7 COSMO-EU COSMO-I7 BIAS 200706-200806 00/24H COSMO-ME COSMO-IT COSMO-I2
COSMO-7 COSMO-EU COSMO-I7 ETS 200706-200806 00/24H COSMO-ME COSMO-IT COSMO-I2
Ticino/valtellina friuli toce veneto trentino garfagnana
COSMO-7 COSMO-EU COSMO-I7 COSMO-ME COSMO-IT COSMO-I2
COSMO-7 COSMO-EU COSMO-I7 COSMO-ME COSMO-IT COSMO-I2