Blanco et al. (2026) On two definitions for precipitation intensity: differences, artifacts and ambiguities
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: Journal of Hydrometeorology
- Year: 2026
- Date: 2026-02-04
- Authors: Joaquin Blanco, Si Cheng, Lisa V. Alexander
- DOI: 10.1175/jhm-d-25-0144.1
Research Groups
Not available in the provided abstract.
Short Summary
This study assesses the differences between two widely used precipitation intensity definitions (I and Iwet) in arid and semi-arid regions using global precipitation data. It finds that I consistently inflates values compared to Iwet, with differences exceeding 100% in arid regions, and advocates for the use of I_wet for more accurate quantification.
Objective
- To assess the differences arising from two widely used precipitation intensity definitions (I and I_wet) and their implications for environmental and infrastructural impacts in arid and semi-arid regions.
Study Configuration
- Spatial Scale: Global, gridded precipitation, with a focus on arid and semi-arid regions.
- Temporal Scale: Daily precipitation rates, averaged over entire analysis periods, and evaluated over two adjacent 20-year periods.
Methodology and Data
- Models used: Comparison of two precipitation intensity definitions:
- I: Average daily precipitation rate over the entire analysis period (P) divided by the frequency of occurrence of wet days (Fwet), where wet days are defined as accumulations of at least 1 mm.
- Iwet: Precipitation rate averaged over wet days only, where wet days are defined as accumulations of at least 1 mm.
- Data sources: Global, gridded precipitation from reanalyses, satellite-derived products, and gauge-derived products.
Main Results
- The precipitation intensity metric I is consistently greater than Iwet (I > Iwet).
- The relative difference between I and Iwet scales inversely with the frequency of wet days (Fwet).
- Over semi-arid regions, the I metric typically inflates values by at least 10% compared to I_wet.
- Over arid regions, the difference between I and I_wet can exceed 100%.
- Singularities were found where I may become larger than the climatological extreme, which is not observed for I_wet.
- The sign of the relative change in intensity from two adjacent 20-year periods can differ depending on whether I or I_wet is used.
- For very arid regions, defining wet days as rates greater than 1 mm may account for smaller precipitation accumulations than "dry" days (less than 1 mm).
- Artifacts can be circumvented by adopting a wet day threshold of 0.1 mm.
- The study advocates for the use of the I_wet metric and emphasizes the need for clear and unambiguous nomenclatures.
Contributions
- Quantifies and highlights significant differences between two common precipitation intensity definitions (I and I_wet), particularly in arid and semi-arid regions.
- Demonstrates that the I metric can substantially inflate precipitation intensity values and even exceed climatological extremes.
- Reveals that the choice of definition can alter the perceived sign of change in precipitation intensity over time.
- Identifies a practical issue with the 1 mm wet day threshold in very arid regions and proposes a solution (0.1 mm threshold).
- Provides a strong recommendation for the use of the I_wet metric and for clearer scientific nomenclature in precipitation studies.
Funding
Not available in the provided abstract.
Citation
@article{Blanco2026two,
author = {Blanco, Joaquin and Cheng, Si and Alexander, Lisa V.},
title = {On two definitions for precipitation intensity: differences, artifacts and ambiguities},
journal = {Journal of Hydrometeorology},
year = {2026},
doi = {10.1175/jhm-d-25-0144.1},
url = {https://doi.org/10.1175/jhm-d-25-0144.1}
}
Original Source: https://doi.org/10.1175/jhm-d-25-0144.1