Will a perfect model agree with perfect observations? The impact of spatial sampling
<p>The spatial resolution of global climate models with interactive aerosol and the observations used to evaluate them is very different. Current models use grid spacings of ∼ 200 km, while satellite observations of aerosol use so-called pixels of ∼ 10 km. Ground site or airborne observation...
| Main Authors: | , , , , , , |
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| Format: | Journal article |
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European Geosciences Union
2016
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| _version_ | 1797077323143446528 |
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| author | Schutgens, N Gryspeerdt, E Weigum, N Tsyro, S Goto, D Schulz, M Stier, P |
| author_facet | Schutgens, N Gryspeerdt, E Weigum, N Tsyro, S Goto, D Schulz, M Stier, P |
| author_sort | Schutgens, N |
| collection | OXFORD |
| description | <p>The spatial resolution of global climate models with interactive aerosol and the observations used to evaluate them is very different. Current models use grid spacings of ∼ 200 km, while satellite observations of aerosol use so-called pixels of ∼ 10 km. Ground site or airborne observations relate to even smaller spatial scales. We study the errors incurred due to different resolutions by aggregating high-resolution simulations (10 km grid spacing) over either the large areas of global model grid boxes ("perfect" model data) or small areas corresponding to the pixels of satellite measurements or the field of view of ground sites ("perfect" observations). Our analysis suggests that instantaneous root-mean-square (RMS) differences of perfect observations from perfect global models can easily amount to 30–160 %, for a range of observables like AOT (aerosol optical thickness), extinction, black carbon mass concentrations, PM2.5, number densities and CCN (cloud condensation nuclei). These differences, due entirely to different spatial sampling of models and observations, are often larger than measurement errors in real observations. Temporal averaging over a month of data reduces these differences more strongly for some observables (e.g. a threefold reduction for AOT), than for others (e.g. a twofold reduction for surface black carbon concentrations), but significant RMS differences remain (10–75 %). Note that this study ignores the issue of temporal sampling of real observations, which is likely to affect our present monthly error estimates. We examine several other strategies (e.g. spatial aggregation of observations, interpolation of model data) for reducing these differences and show their effectiveness. Finally, we examine consequences for the use of flight campaign data in global model evaluation and show that significant biases may be introduced depending on the flight strategy used.</p> |
| first_indexed | 2024-03-07T00:16:19Z |
| format | Journal article |
| id | oxford-uuid:7af6e6f4-3379-4d77-9a67-d2c1086ec3b3 |
| institution | University of Oxford |
| last_indexed | 2024-03-07T00:16:19Z |
| publishDate | 2016 |
| publisher | European Geosciences Union |
| record_format | dspace |
| spelling | oxford-uuid:7af6e6f4-3379-4d77-9a67-d2c1086ec3b32022-03-26T20:47:33ZWill a perfect model agree with perfect observations? The impact of spatial samplingJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:7af6e6f4-3379-4d77-9a67-d2c1086ec3b3Symplectic Elements at OxfordEuropean Geosciences Union2016Schutgens, NGryspeerdt, EWeigum, NTsyro, SGoto, DSchulz, MStier, P<p>The spatial resolution of global climate models with interactive aerosol and the observations used to evaluate them is very different. Current models use grid spacings of ∼ 200 km, while satellite observations of aerosol use so-called pixels of ∼ 10 km. Ground site or airborne observations relate to even smaller spatial scales. We study the errors incurred due to different resolutions by aggregating high-resolution simulations (10 km grid spacing) over either the large areas of global model grid boxes ("perfect" model data) or small areas corresponding to the pixels of satellite measurements or the field of view of ground sites ("perfect" observations). Our analysis suggests that instantaneous root-mean-square (RMS) differences of perfect observations from perfect global models can easily amount to 30–160 %, for a range of observables like AOT (aerosol optical thickness), extinction, black carbon mass concentrations, PM2.5, number densities and CCN (cloud condensation nuclei). These differences, due entirely to different spatial sampling of models and observations, are often larger than measurement errors in real observations. Temporal averaging over a month of data reduces these differences more strongly for some observables (e.g. a threefold reduction for AOT), than for others (e.g. a twofold reduction for surface black carbon concentrations), but significant RMS differences remain (10–75 %). Note that this study ignores the issue of temporal sampling of real observations, which is likely to affect our present monthly error estimates. We examine several other strategies (e.g. spatial aggregation of observations, interpolation of model data) for reducing these differences and show their effectiveness. Finally, we examine consequences for the use of flight campaign data in global model evaluation and show that significant biases may be introduced depending on the flight strategy used.</p> |
| spellingShingle | Schutgens, N Gryspeerdt, E Weigum, N Tsyro, S Goto, D Schulz, M Stier, P Will a perfect model agree with perfect observations? The impact of spatial sampling |
| title | Will a perfect model agree with perfect observations? The impact of spatial sampling |
| title_full | Will a perfect model agree with perfect observations? The impact of spatial sampling |
| title_fullStr | Will a perfect model agree with perfect observations? The impact of spatial sampling |
| title_full_unstemmed | Will a perfect model agree with perfect observations? The impact of spatial sampling |
| title_short | Will a perfect model agree with perfect observations? The impact of spatial sampling |
| title_sort | will a perfect model agree with perfect observations the impact of spatial sampling |
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