BALTEX water and energy budgets in the NCEP/DOE reanalysis II

Water and energy budgets from the National Centers for Environmental Prediction/Dept. of Energy (NCEP/DOE) reanalysis II (NCEPRII) are described for the Baltic Sea catchment and sea (BALTEX). Annually, NCEPRII shows 0.7 mm d–1 of atmospheric moisture converged into the land region with a corresponding runoff of 0.7 mm d–1 to the Baltic Sea, consistent with observations. However, precipitation is too low; evaporation is too large; runoff does not have an appropriate winter minimum and spring maximum; the assimilation and surface nudging are too large. Important hydroclimatic characteristics can still be discerned. During summer, atmospheric water vapor, precipitation, evaporation, and surface and atmospheric radiative heating increase and the atmospheric radiative cooling, dry static energy convergence decrease. There are large contrasts between the sea and land; during winter sensible heat is transferred from the sea to the atmosphere and sea evaporation and precipitation are largest during the fall and winter; somewhat opposite behavior occurs over land.

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Publication Details

Journal
Boreal Environment Research Journal Archive
Published
2024-12-12
DOI
https://doi.org/10.60910/96t9-bq1c
Citations
1
Primary Topic
Climate variability and models
Type
article
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article

BALTEX water and energy budgets in the NCEP/DOE reanalysis II

E. Raschke, Burkhardt Rockel
1 citations
Boreal Environment Research Journal Archive
Climate variability and models
article

BALTEX water and energy budgets in the NCEP/DOE reanalysis II

E. Raschke, Burkhardt Rockel
article en
1 citations

Abstract

Water and energy budgets from the National Centers for Environmental Prediction/Dept. of Energy (NCEP/DOE) reanalysis II (NCEPRII) are described for the Baltic Sea catchment and sea (BALTEX). Annually, NCEPRII shows 0.7 mm d–1 of atmospheric moisture converged into the land region with a corresponding runoff of 0.7 mm d–1 to the Baltic Sea, consistent with observations. However, precipitation is too low; evaporation is too large; runoff does not have an appropriate winter minimum and spring maximum; the assimilation and surface nudging are too large. Important hydroclimatic characteristics can still be discerned. During summer, atmospheric water vapor, precipitation, evaporation, and surface and atmospheric radiative heating increase and the atmospheric radiative cooling, dry static energy convergence decrease. There are large contrasts between the sea and land; during winter sensible heat is transferred from the sea to the atmosphere and sea evaporation and precipitation are largest during the fall and winter; somewhat opposite behavior occurs over land.

Boreal Environment Research Journal Archive
Openalex Percentile: Top 100%
Climate variability and models
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BALTEX water and energy budgets in the NCEP/DOE reanalysis II — E. Raschke, Burkhardt Rockel · Boreal Environment Research Journal Archive (2024) | TGRS Research Map | TGRS