Evidence map›Paper›PMID 34163306›Full record

ArticleJournal of hydrometeorology2020

Object-Based Comparison of Data-Driven and Physics-Driven Satellite Estimates of Extreme Rainfall.

Zhe Li, Daniel B Wright, Sara Q Zhang, Dalia B Kirschbaum, Samantha H Hartke

Abstract read
In one paragraph

Article in Journal of hydrometeorology, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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0citing papers in PubMed
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1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

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3 · Its place in the literature

Who cites it

0 citing papers in PubMed.

No citing paper in PubMed yet.

4 · The record

Corrections and comments

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5 · Who and what money

Authors and funding

5 authors.

Zhe LiDepartment of Civil and Environmental Engineering, University of Wisconsin-Madison, Madison, Wisconsin.
Daniel B WrightDepartment of Civil and Environmental Engineering, University of Wisconsin-Madison, Madison, Wisconsin.
Sara Q ZhangNASA Goddard Space Flight Center, Greenbelt, Maryland.
Dalia B KirschbaumNASA Goddard Space Flight Center, Greenbelt, Maryland.
Samantha H HartkeDepartment of Civil and Environmental Engineering, University of Wisconsin-Madison, Madison, Wisconsin.

Funding

Shared Services Center NASA 80NSSC18K1321Shared Services Center NASA 80NSSC19K0726
6 · The paper itself

Abstract

The Global Precipitation Measurement (GPM) constellation of spaceborne sensors provides a variety of direct and indirect measurements of precipitation processes. Such observations can be employed to derive spatially and temporally consistent gridded precipitation estimates either via data-driven retrieval algorithms or by assimilation into physically based numerical weather models. We compare the data-driven Integrated Multisatellite Retrievals for GPM (IMERG) and the assimilation-enabled NASA-Unified Weather Research and Forecasting (NU-WRF) model against Stage IV reference precipitation for four major extreme rainfall events in the southeastern United States using an object-based analysis framework that decomposes gridded precipitation fields into storm objects. As an alternative to conventional "grid-by-grid analysis," the object-based approach provides a promising way to diagnose spatial properties of storms, trace them through space and time, and connect their accuracy to storm types and input data sources. The evolution of two tropical cyclones are generally captured by IMERG and NU-WRF, while the less organized spatial patterns of two mesoscale convective systems pose challenges for both. NU-WRF rain rates are generally more accurate, while IMERG better captures storm location and shape. Both show higher skill in detecting large, intense storms compared to smaller, weaker storms. IMERG's accuracy depends on the input microwave and infrared data sources; NU-WRF does not appear to exhibit this dependence. Findings highlight that an object-oriented view can provide deeper insights into satellite precipitation performance and that the satellite precipitation community should further explore the potential for "hybrid" data-driven and physics-driven estimates in order to make optimal usage of satellite observations.

Indexed as

Extreme eventsNumerical weather prediction/forecastingPrecipitationRemote sensingSatellite observations

Identifiers

PMID34163306
PMCPMC8216224

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.