Effect of boundary conditions on adjoint-based forecast sensitivity observation impact in a regional model

Hyun Mee Kim, Dae Hui Kim

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1 Citation (Scopus)

Abstract

In this study, the effect of boundary-condition configurations in the regional Weather Research and Forecasting (WRF) Model on the adjoint-based forecast sensitivity observation impact (FSOI) for 24 h forecast error reduction was evaluated. The FSOI has been used to diagnose the impact of observations on the forecast performance in several global and regional models. Different from the global model, in the regional model, the lateral boundaries affect forecasts and FSOI results. Several experiments with different lateral boundary conditions were conducted. The experi-mental period was from 1 to 14 June 2015. With or without data assimilation, the larger the buffer size in lateral boundary conditions, the smaller the forecast error. The nonlinear and linear forecast error reduction (i.e., observation impact) decreased as the buffer size increased, implying larger impact of lateral boundaries and smaller observation impact on the forecast error. In most experiments, in terms of observation types (variables), upper-air radiosonde observations (brightness temperature) exhibited the greatest observation impact. The ranking of observation impacts was consistent for observation types and variables among experiments with a constraint in the response function at the upper boundary. The fractions of beneficial observations were approximately 60%, and did not considerably vary depending on the boundary conditions specified when calculating the FSOI in the regional modeling framework.

Original languageEnglish
Pages (from-to)1233-1247
Number of pages15
JournalJournal of Atmospheric and Oceanic Technology
Volume38
Issue number7
DOIs
Publication statusPublished - 2021

Bibliographical note

Funding Information:
This study was supported by a National Research Foundation of Korea (NRF) grant funded by the South Korean government (Ministry of Science and ICT) (Grant 2021R1A2C1012572) and the Yonsei Signature Research Cluster Program of 2021 (2021-22-0003). The simulations were primarily conducted by utilizing the supercomputer system supported by the National Center for Meteorological Supercomputer of the Korea Meteorological Administration (KMA). Additionally, the authors appreciate Myunghwan Kim and Dr. Sung-Min Kim for their earlier work associated with this study.

Funding Information:
Acknowledgments. This study was supported by a National Research Foundation of Korea (NRF) grant funded by the South Korean government (Ministry of Science and ICT) (Grant 2021R1A2C1012572) and the Yonsei Signature Research Cluster Program of 2021 (2021-22-0003). The simulations were primarily conducted by utilizing the supercomputer system supported by the National Center for Meteorological Supercomputer of the Korea Meteorological Administration (KMA). Additionally, the authors appreciate Myunghwan Kim and Dr. Sung-Min Kim for their earlier work associated with this study.

Publisher Copyright:
© 2021 American Meteorological Society.

All Science Journal Classification (ASJC) codes

  • Ocean Engineering
  • Atmospheric Science

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