2020
DOI: 10.1002/essoar.10503422.1
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TROPOMI NO2 in the United States: A detailed look at the annual averages, weekly cycles, effects of temperature, and correlation with PM2.5

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Cited by 25 publications
(19 citation statements)
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“…However, when the normalized data are smoothed with 28‐day rolling mean values, the correlation improved with a correlation coefficient of 0.75 for both the pre‐lockdown and the lockdown/post‐lockdown periods (Figures 4e and 4f). This is consistent with other studies involving satellite tropNO 2 data where 28‐day rolling means or weekly averaging was carried out to minimize noise and data gaps (Goldberg et al., 2021; Misra et al., 2021).…”
Section: Resultssupporting
confidence: 90%
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“…However, when the normalized data are smoothed with 28‐day rolling mean values, the correlation improved with a correlation coefficient of 0.75 for both the pre‐lockdown and the lockdown/post‐lockdown periods (Figures 4e and 4f). This is consistent with other studies involving satellite tropNO 2 data where 28‐day rolling means or weekly averaging was carried out to minimize noise and data gaps (Goldberg et al., 2021; Misra et al., 2021).…”
Section: Resultssupporting
confidence: 90%
“…(2020) report that the Los Angeles basin was unusually wet in 2020, especially during the late March and early April 2020. Other researchers who correlated daily surface observations of NO 2 and TROPOMI tropNO 2 for 35 different stations in Europe reported similar findings and they found that correlation improved after averaging the data to monthly time scales (Cersosimo et al., 2020; Goldberg et al., 2021; Ialongo et al., 2020). The comparison for the lockdown and post‐lockdown period of March through November is shown in Figure 4b; the correlation remains the same ( r = 0.39) but the one interesting feature is that the tropNO 2 and on‐road emissions are very small during the lockdown compared to the pre‐lockdown.…”
Section: Resultsmentioning
confidence: 59%
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“…Observations with retrieved cloud fractions greater than 0.1 or flagged as poor quality or snow-covered (that is, TROPOMI quality assurance flag <0.75) are excluded. Although the resolution of TROPOMI observations is 3.5 × 5.5 km 2 , several studies have demonstrated that oversampling techniques can provide accurate NO 2 maps at 1 × 1 km 2 resolution when averaging over a one-month period 31,32,54 . An area-weighted oversampling technique 55,56 is used to map daily satellite NO 2 column observations from TROPOMI onto a ~0.01° × 0.01° (~1 × 1 km 2 ) resolution grid and from OMI to a 0.1° × 0.125° (~10 × 10 km 2 ) grid, as these resolutions balance the need of fine resolution for observing fine-scale structure and of minimizing the effects of sampling biases and noise in the observations.…”
Section: Datamentioning
confidence: 99%
“…The newest remote sensing spectrometer, the European Space Agency's TROPOspheric Monitoring Instrument (TROPOMI) 30 on the Copernicus Sentinel 5p satellite, has been providing NO 2 observations with finer spatial resolution and higher instrument sensitivity since 2018. These attributes allow the generation of TROPOMI NO 2 maps at 100 times finer resolution (approximately 1 × 1 km 2 ) with a one-month averaging period 31,32 , an improvement over the spatial and temporal averaging needed for accurate OMI maps (typically approximately 10 × 10 km 2 over one year) 24 . Concurrently, the excellent stability of the OMI instrument over the last 15 years provides an ideal dataset for long-term trend analysis 28,33 that offers context for recent TROPOMI data.…”
mentioning
confidence: 99%