@Article{SilvaHodgCout:2021:HoWeDo,
author = "Silva, Philipp Edson Dias da and Hodges, Kevin Ivan and Coutinho,
Mariane Mendes",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {University
of Reading} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "How well does the HadGEM2-ES coupled model represent the Southern
Hemisphere storm tracks?",
journal = "Climate Dynamics",
year = "2021",
volume = "56",
number = "3/4",
pages = "1145--1162",
month = "Feb.",
keywords = "Cyclones, Storm tracks, Climatology, HadGEM2-ES, ERA-Interim,
Southern Hemisphere.",
abstract = "This study presents an assessment of the ability of the Hadley
Centre Global Environment Model version 2-Earth system
configuration (HadGEM2-ES)-in simulating the mid-latitude storm
tracks over the Southern Hemisphere (SH). The storm tracks are
primarily assessed using cyclone tracking using data from a 4
member ensemble of 27-year simulations of HadGEM2-ES over the
historical period, and the European Centre for Medium-Range
Weather Forecasts Interim Reanalysis. Both winter and summer
periods are considered and contrasted. Results show that the storm
track (ST) climatology of HadGEM2-ES presents similar patterns to
those of the reanalysis. However, the model tends to represent the
austral winter ST position with an equatorward bias and a zonal
bias in the spiral towards the pole. The main differences were
found during the austral winter, with large track density biases
over the Indian Ocean indicating a poor representation of the ST
in this specific region. This was found to be related to two
factors. First, the large negative genesis biases over South
America, Antarctic Peninsula and the Antarctic coast. Second, the
model resolution and the representation of the Andes Mountains in
South America. The link between STs and the large-scale
circulation is examined and shows at upper levels an equatorward
jet position bias of the subtropical jet and a negative bias in
the eddy-driven, associated with a large cold bias over the
extratropical and polar regions. The analysis of the large-scale
circulation shows that the split jet during winter has problems in
the model linked to these biases, including geopotential anomaly
and sea surface temperature biases. Consequently, in general the
track densities over the Southern oceans are underestimated in the
austral winter. During summer, the results show the STs move
poleward and there is a single eddy-driven jet, which is
represented relatively well compared with the winter situation.
These factors tend to reduce the differences seen in the cyclone
track distribution biases. Although the model has biases in the ST
behaviour in the SH it is still considered that these do not
preclude this model being used for perturbation and future
projection studies.",
doi = "10.1007/s00382-020-05523-9",
url = "http://dx.doi.org/10.1007/s00382-020-05523-9",
issn = "0930-7575",
language = "en",
targetfile = "silva_how.pdf",
urlaccessdate = "29 jun. 2024"
}