On the (In)Homogeneity of Reanalysis ProductsSource: Journal of Climate:;2004:;volume( 017 ):;issue: 019::page 3866Author:Sterl, Andreas
DOI: 10.1175/1520-0442(2004)017<3866:OTIORP>2.0.CO;2Publisher: American Meteorological Society
Abstract: The homogeneity of the ECMWF 40-yr Re-Analysis (ERA-40) is assessed. This is done by comparing ERA-40 data with results from the NCEP?NCAR reanalysis and also by investigating a known relationship between a modeled (latent heat flux) and an external (SST) quantity. The direct comparison between the two reanalyses reveals a lot of inhomogeneities. They occur mainly in the Southern Hemisphere and before 1980. While observational density was sufficient to effectively constrain the models in the Northern Hemisphere, it was not in the Southern Hemisphere. From the investigation of the relationship between latent heat flux and SST it is found that, because of an increasing amount of data, the reanalysis results become more reliable toward the end of the reanalysis period (approximately after 1980). When using the reanalysis data to investigate climate change issues care has to be taken not to confuse the inhomogeneities with real changes.
|
Collections
Show full item record
contributor author | Sterl, Andreas | |
date accessioned | 2017-06-09T16:24:40Z | |
date available | 2017-06-09T16:24:40Z | |
date copyright | 2004/10/01 | |
date issued | 2004 | |
identifier issn | 0894-8755 | |
identifier other | ams-6736.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4208800 | |
description abstract | The homogeneity of the ECMWF 40-yr Re-Analysis (ERA-40) is assessed. This is done by comparing ERA-40 data with results from the NCEP?NCAR reanalysis and also by investigating a known relationship between a modeled (latent heat flux) and an external (SST) quantity. The direct comparison between the two reanalyses reveals a lot of inhomogeneities. They occur mainly in the Southern Hemisphere and before 1980. While observational density was sufficient to effectively constrain the models in the Northern Hemisphere, it was not in the Southern Hemisphere. From the investigation of the relationship between latent heat flux and SST it is found that, because of an increasing amount of data, the reanalysis results become more reliable toward the end of the reanalysis period (approximately after 1980). When using the reanalysis data to investigate climate change issues care has to be taken not to confuse the inhomogeneities with real changes. | |
publisher | American Meteorological Society | |
title | On the (In)Homogeneity of Reanalysis Products | |
type | Journal Paper | |
journal volume | 17 | |
journal issue | 19 | |
journal title | Journal of Climate | |
identifier doi | 10.1175/1520-0442(2004)017<3866:OTIORP>2.0.CO;2 | |
journal fristpage | 3866 | |
journal lastpage | 3873 | |
tree | Journal of Climate:;2004:;volume( 017 ):;issue: 019 | |
contenttype | Fulltext |