Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory
Boundary layer moisture variability at the Eastern North Atlantic (ENA) site is examined at monthly and daily time scales using 5 years of ground-based observations and output from European Center for Medium range Weather Forecast (ECMWF) reanalysis model. The annual cycle of the mixed layer water b...
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ftcopernicus:oai:publications.copernicus.org:acpd106094 2023-05-15T17:31:04+02:00 Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory Cadeddu, Maria Paola Ghate, Virendra Turner, David Surleta, Thomas 2022-09-01 application/pdf https://doi.org/10.5194/acp-2022-615 https://acp.copernicus.org/preprints/acp-2022-615/ eng eng doi:10.5194/acp-2022-615 https://acp.copernicus.org/preprints/acp-2022-615/ eISSN: 1680-7324 Text 2022 ftcopernicus https://doi.org/10.5194/acp-2022-615 2022-09-05T16:22:54Z Boundary layer moisture variability at the Eastern North Atlantic (ENA) site is examined at monthly and daily time scales using 5 years of ground-based observations and output from European Center for Medium range Weather Forecast (ECMWF) reanalysis model. The annual cycle of the mixed layer water budgets is presented to estimate the relative contribution of large-scale advection, local moisture tendency, entrainment, and precipitation to balance the moistening due to surface latent heat flux on monthly timescales. Advection of colder and dry air from the North acts as an important moisture sink (~ 50 % of the overall budget) during fall and winter driving the seasonality of the budget. Entrainment and precipitation contribute to the drying of the boundary layer (~25 % and ~15 % respectively) and the local change in moisture contributes to a small residual part. On a daily temporal scale, moist and dry mesoscale columns of vapor (~10 km) are analyzed during 10 selected days of precipitating stratocumulus clouds. Adjacent moist and dry columns present distinct mesoscale features that are strongly correlated with clouds and precipitation. Dry columns adjacent to moist columns have more frequent and stronger downdrafts immediately below the cloud base. Moist columns have more frequent updrafts, stronger cloud top cooling, higher liquid water path and precipitation compared to the dry columns. This study highlights the complex interaction between large-scale and local processes controlling the boundary layer moisture and the importance of vapor spatial distribution to support convection and precipitation. Text North Atlantic Copernicus Publications: E-Journals |
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Copernicus Publications: E-Journals |
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language |
English |
description |
Boundary layer moisture variability at the Eastern North Atlantic (ENA) site is examined at monthly and daily time scales using 5 years of ground-based observations and output from European Center for Medium range Weather Forecast (ECMWF) reanalysis model. The annual cycle of the mixed layer water budgets is presented to estimate the relative contribution of large-scale advection, local moisture tendency, entrainment, and precipitation to balance the moistening due to surface latent heat flux on monthly timescales. Advection of colder and dry air from the North acts as an important moisture sink (~ 50 % of the overall budget) during fall and winter driving the seasonality of the budget. Entrainment and precipitation contribute to the drying of the boundary layer (~25 % and ~15 % respectively) and the local change in moisture contributes to a small residual part. On a daily temporal scale, moist and dry mesoscale columns of vapor (~10 km) are analyzed during 10 selected days of precipitating stratocumulus clouds. Adjacent moist and dry columns present distinct mesoscale features that are strongly correlated with clouds and precipitation. Dry columns adjacent to moist columns have more frequent and stronger downdrafts immediately below the cloud base. Moist columns have more frequent updrafts, stronger cloud top cooling, higher liquid water path and precipitation compared to the dry columns. This study highlights the complex interaction between large-scale and local processes controlling the boundary layer moisture and the importance of vapor spatial distribution to support convection and precipitation. |
format |
Text |
author |
Cadeddu, Maria Paola Ghate, Virendra Turner, David Surleta, Thomas |
spellingShingle |
Cadeddu, Maria Paola Ghate, Virendra Turner, David Surleta, Thomas Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory |
author_facet |
Cadeddu, Maria Paola Ghate, Virendra Turner, David Surleta, Thomas |
author_sort |
Cadeddu, Maria Paola |
title |
Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory |
title_short |
Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory |
title_full |
Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory |
title_fullStr |
Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory |
title_full_unstemmed |
Boundary layer moisture variability at the ARM Eastern North Atlantic Observatory |
title_sort |
boundary layer moisture variability at the arm eastern north atlantic observatory |
publishDate |
2022 |
url |
https://doi.org/10.5194/acp-2022-615 https://acp.copernicus.org/preprints/acp-2022-615/ |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-2022-615 https://acp.copernicus.org/preprints/acp-2022-615/ |
op_doi |
https://doi.org/10.5194/acp-2022-615 |
_version_ |
1766128372586381312 |