A Spatiotemporal Water Vapor–Deep Convection Correlation Metric Derived from the Amazon Dense GNSS Meteorological NetworkSource: Monthly Weather Review:;2016:;volume( 145 ):;issue: 001::page 279DOI: 10.1175/MWR-D-16-0140.1Publisher: American Meteorological Society
Abstract: eep atmospheric convection, which covers a large range of spatial scales during its evolution, continues to be a challenge for models to replicate, particularly over land in the tropics. Specifically, the shallow-to-deep convective transition and organization on the mesoscale are often not properly represented in coarse-resolution models. High-resolution models offer insights on physical mechanisms responsible for the shallow-to-deep transition. Model verification, however, at both coarse and high resolution requires validation and, hence, observational metrics, which are lacking in the tropics. Here a straightforward metric derived from the Amazon Dense GNSS Meteorological Network (~100 km ? 100 km) is presented based on a spatial correlation decay time scale during convective evolution on the mesoscale. For the shallow-to-deep transition, the correlation decay time scale is shown to be around 3.5 h. This novel result provides a much needed metric from the deep tropics for numerical models to replicate.
|
Collections
Show full item record
contributor author | Adams, David K. | |
contributor author | Barbosa, Henrique M. J. | |
contributor author | Gaitán De Los Ríos, Karen Patricia | |
date accessioned | 2017-06-09T17:34:08Z | |
date available | 2017-06-09T17:34:08Z | |
date copyright | 2017/01/01 | |
date issued | 2016 | |
identifier issn | 0027-0644 | |
identifier other | ams-87329.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4230986 | |
description abstract | eep atmospheric convection, which covers a large range of spatial scales during its evolution, continues to be a challenge for models to replicate, particularly over land in the tropics. Specifically, the shallow-to-deep convective transition and organization on the mesoscale are often not properly represented in coarse-resolution models. High-resolution models offer insights on physical mechanisms responsible for the shallow-to-deep transition. Model verification, however, at both coarse and high resolution requires validation and, hence, observational metrics, which are lacking in the tropics. Here a straightforward metric derived from the Amazon Dense GNSS Meteorological Network (~100 km ? 100 km) is presented based on a spatial correlation decay time scale during convective evolution on the mesoscale. For the shallow-to-deep transition, the correlation decay time scale is shown to be around 3.5 h. This novel result provides a much needed metric from the deep tropics for numerical models to replicate. | |
publisher | American Meteorological Society | |
title | A Spatiotemporal Water Vapor–Deep Convection Correlation Metric Derived from the Amazon Dense GNSS Meteorological Network | |
type | Journal Paper | |
journal volume | 145 | |
journal issue | 1 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/MWR-D-16-0140.1 | |
journal fristpage | 279 | |
journal lastpage | 288 | |
tree | Monthly Weather Review:;2016:;volume( 145 ):;issue: 001 | |
contenttype | Fulltext |