CONUS404: Precip overestimation over urban areas #402
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Dear Michelle, We know how to improve the representation of urban areas in our simulation and implement them into simulations that focus on the Delaware River basin. We plan to implement these changes into future CONUS simulations. I also found an underestimation of 10 m wind in the CONUS404 simulations (e.g., see Fig. 2 in the supplement of this paper). However, I am not sure how strong this is related to biases in ERA5. Please let me know if you have any additional questions. All the best, |
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From Figure 4 of the CONUS404 publication (Rasmussen et al., 2023) it is evident that CONUS404 is overestimating convective precipitation over urban centers. Any idea why that might be and what model parameters (if any) could be tweaked to avoid that? We know that PRISM might not be perfect but, at least for Florida, the average annual precipitation of 100 inches/year simulated by CONUS404 over the Miami-WPB urban areas is way too high. Precipitation is overestimated over other urban areas in FL as well, but not as drastically as over Miami-WPB.
There are studies that show that the UHI enhances wet season precipitation over urban centers and areas downwind. A study by Marshall and others (2004) indicates that "increased sea-breeze convergence and small increases in convective precipitation over urban areas along the eastern coastal ridge of south Florida [Miami-WPB area] are caused by increased sensible heat flux, which appears related to urbanization during the period 1900-93." I understand this, but it seems like this effect might be overestimated in CONUS404.
I have also noticed that ERA5 wind speeds at 10 m have a low bias and this is translating into a low bias in CONUS404 10-m wind speeds over Florida (CONUS404 nudges to ERA5 winds above the PBL). A low bias in ERA5 wind speeds is very well known (at least over the oceans). Could the lower surface wind speeds be affecting precipitation over urban areas?
Thanks for any insights on the above.
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