Impact of More Frequent Observations on the Understanding of Tasmanian Fire DangerSource: Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 008::page 1617Author:Fox-Hughes, Paul
DOI: 10.1175/JAMC-D-10-05001.1Publisher: American Meteorological Society
Abstract: alf-hourly airport weather observations have been used to construct high-temporal-resolution datasets of McArthur Mark V forest fire danger index (FFDI) values for three locations in Tasmania, Australia, enabling a more complete understanding of the range and diurnal variability of fire weather. Such an understanding is important for fire management and planning to account for the possibility of weather-related fire flare ups?in particular, early in a day and during rapidly changing situations. In addition, climate studies have hitherto generally been able to access only daily or at best 3-hourly weather data to generate fire-weather index values. Comparison of FFDI values calculated from frequent (subhourly) observations with those derived from 3-hourly synoptic observations suggests that large numbers of significant fire-weather events are missed, even by a synoptic observation schedule, and, in particular, by observations made at 1500 LT only, suggesting that many climate studies may underestimate the frequencies of occurrence of fire-weather events. At Hobart, in southeastern Tasmania, only one-half of diurnal FFDI peaks over a critical warning level occur at 1500 LT, with the remainder occurring across a broad range of times. The study reinforces a perception of pronounced differences in the character of fire weather across Tasmania, with differences in diurnal patterns of variability evident between locations, in addition to well-known differences in the ranges of peak values observed.
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contributor author | Fox-Hughes, Paul | |
date accessioned | 2017-06-09T16:48:24Z | |
date available | 2017-06-09T16:48:24Z | |
date copyright | 2011/08/01 | |
date issued | 2011 | |
identifier issn | 1558-8424 | |
identifier other | ams-74490.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4216720 | |
description abstract | alf-hourly airport weather observations have been used to construct high-temporal-resolution datasets of McArthur Mark V forest fire danger index (FFDI) values for three locations in Tasmania, Australia, enabling a more complete understanding of the range and diurnal variability of fire weather. Such an understanding is important for fire management and planning to account for the possibility of weather-related fire flare ups?in particular, early in a day and during rapidly changing situations. In addition, climate studies have hitherto generally been able to access only daily or at best 3-hourly weather data to generate fire-weather index values. Comparison of FFDI values calculated from frequent (subhourly) observations with those derived from 3-hourly synoptic observations suggests that large numbers of significant fire-weather events are missed, even by a synoptic observation schedule, and, in particular, by observations made at 1500 LT only, suggesting that many climate studies may underestimate the frequencies of occurrence of fire-weather events. At Hobart, in southeastern Tasmania, only one-half of diurnal FFDI peaks over a critical warning level occur at 1500 LT, with the remainder occurring across a broad range of times. The study reinforces a perception of pronounced differences in the character of fire weather across Tasmania, with differences in diurnal patterns of variability evident between locations, in addition to well-known differences in the ranges of peak values observed. | |
publisher | American Meteorological Society | |
title | Impact of More Frequent Observations on the Understanding of Tasmanian Fire Danger | |
type | Journal Paper | |
journal volume | 50 | |
journal issue | 8 | |
journal title | Journal of Applied Meteorology and Climatology | |
identifier doi | 10.1175/JAMC-D-10-05001.1 | |
journal fristpage | 1617 | |
journal lastpage | 1626 | |
tree | Journal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 008 | |
contenttype | Fulltext |