Relationship between MODIS fire hot spot count and burned area in a degraded tropical peat swamp forest in Central Kalimantan, Indonesia

被引:72
作者
Tansey, K. [1 ]
Beston, J. [1 ]
Hoscilo, A. [1 ]
Page, S. E. [1 ]
Hernandez, C. U. Paredes [1 ]
机构
[1] Univ Leicester, Dept Geog, Leicester LE1 7RH, Leics, England
关键词
D O I
10.1029/2008JD010717
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A number of space-borne sensors observe radiant energy at thermal wavelengths. Thermal anomaly data, otherwise known as hotspot data, have been shown to be particularly correlated with the occurrence of active fires (a fire normally with a flaming component and/or smoldering component). Because of a lack of high-quality burned area data, recent studies have used hotspot data as a proxy for burned area when calculating gas emissions or atmospheric pollutants as a result of biomass burning. We argue that the relationship between hotspot data and burned area is spatially variable and strongly dependent on the vegetation type and function. In this article, we explore the relationship between hotspot data and burned area for a region of degraded and partially altered tropical peat swamp forest in southern Kalimantan, Indonesia. MODIS thermal anomaly (MOD14A1) data were used, alongside disaster monitoring constellation (DMC) and Landsat TM data that were used to derive the burnt area, to calculate a figure indicating the average burned area per hotspot (A(R)). Two different levels of hotspot detection confidence are examined in order to ascertain which confidence levels best describe fires in a tropical peat swamp forest environment. Only a relatively small number of fires were detected at the lowest confidence level, but these small number of hotspots improved results. Results for the estimation of burnt area for each hotspot were found to vary between 15 and 16 ha. Omission errors are of the order of 60%; hotspot commission rates are of the order of 8%.
引用
收藏
页数:8
相关论文
共 52 条
[1]   Emission of trace gases and aerosols from biomass burning [J].
Andreae, MO ;
Merlet, P .
GLOBAL BIOGEOCHEMICAL CYCLES, 2001, 15 (04) :955-966
[2]  
[Anonymous], 2006, ATMOSPHERIC CHEM PHY, DOI DOI 10.5194/ACPD-6-9655-2006
[3]   Assessment of different spectral indices in the red-near-infrared spectral domain for burned land discrimination [J].
Chuvieco, E ;
Martín, MP ;
Palacios, A .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 2002, 23 (23) :5103-5110
[4]   Generation of long time series of burn area maps of the boreal forest from NOAA-AVHRR composite data [J].
Chuvieco, Emilio ;
Englefield, Peter ;
Trishchenko, Alexander P. ;
Luo, Yi .
REMOTE SENSING OF ENVIRONMENT, 2008, 112 (05) :2381-2396
[5]   Comparison of burn severity assessments using Differenced Normalized Burn Ratio and ground data [J].
Cocke, AE ;
Fulé, PZ ;
Crouse, JE .
INTERNATIONAL JOURNAL OF WILDLAND FIRE, 2005, 14 (02) :189-198
[6]   BIOMASS BURNING IN THE TROPICS - IMPACT ON ATMOSPHERIC CHEMISTRY AND BIOGEOCHEMICAL CYCLES [J].
CRUTZEN, PJ ;
ANDREAE, MO .
SCIENCE, 1990, 250 (4988) :1669-1678
[7]   Validation of active fire detection from moderate-resolution satellite sensors: The MODIS example in northern Eurasia [J].
Csiszar, Ivan A. ;
Morisette, Jeffrey T. ;
Giglio, Louis .
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, 2006, 44 (07) :1757-1764
[8]   Hemolysin production by Staphylococcus aureus species isolated from mastitic goat milk in Brazilian dairy herds [J].
da Silva, ER ;
Boechat, JUD ;
Martins, JCD ;
Ferreira, WPB ;
Siqueira, AP ;
da Silva, N .
SMALL RUMINANT RESEARCH, 2005, 56 (1-3) :271-275
[9]   Global spatial and temporal distribution of vegetation fire as determined from satellite observations [J].
Dwyer, E ;
Pinnock, S ;
Grégoire, JM ;
Pereira, JMC .
INTERNATIONAL JOURNAL OF REMOTE SENSING, 2000, 21 (6-7) :1289-1302
[10]   Evaluation of remotely sensed indices for assessing burn severity in interior Alaska using Landsat TM and ETM+ [J].
Epting, J ;
Verbyla, D ;
Sorbel, B .
REMOTE SENSING OF ENVIRONMENT, 2005, 96 (3-4) :328-339