These authors contributed equally to this work.
Wildfires have a strong negative effect on the environment, ecology
and public health. However, the potential degradation of mainstream global
fire products leads to large uncertainty in the effective monitoring of wildfires and their influence. To fill this gap, we produced Fengyun-3D (FY-3D) global fire
products with a similar spatial and temporal resolution, aiming to serve as
an alternative to and continuity for Moderate Resolution Imaging Spectroradiometer (MODIS) global fire products. Firstly, the
sensor parameters and major algorithms for noise detection and fire
identification in FY-3D products were introduced. For visual-check-based
accuracy assessment, five typical regions with a large number of fire spots across the globe, Africa, South America, the Indochinese
Peninsula, Siberia and Australia, were selected, and the
overall accuracy exceeded 94 %. Meanwhile, the consistence between FY-3D
and MODIS fire products was examined. The result suggested that the overall
consistence was 84.4 %, with a fluctuation across seasons, surface types
and regions. The high accuracy and consistence with MODIS products proved
that the FY-3D fire product is an ideal tool for global fire monitoring. Based
on field-collected reference data, we further evaluated the suitability of
FY-3D fire products in China. The overall accuracy and accuracy without
considering omission errors were 79.43 % and 88.50 %
higher, respectively, than those of MODIS fire products. Since detailed local geographical
conditions were specifically considered, FY-3D products should be preferably
employed for fire monitoring in China. The FY-3D fire dataset can be downloaded at
More than half of global land surfaces have been influenced by wildfires, and the total global burned area adds up to the area of the European Union every year (Andela et al., 2019; Keeley et al., 2011; Moritz et al., 2012). Wildfires, especially large-scale wildfires, in forests, grasslands and farmlands, have a significant impact on crop productivity (Jethva et al., 2019), atmospheric pollution (Guo et al., 2020), biodiversity (Kelly et al., 2020), climate change (Alisjahbana and Busch, 2017; Keegan et al., 2014) and public health (Huff et al., 2015; Johnston et al., 2012; Oliveira et al., 2020; Yuchi et al., 2016). In recent years, the increasing events of forest fires in China, the USA, Australia, and Amazon rain forests and grassland fires in Mongolia have caused a large number of casualties (Cochrane, 2003), the loss of millions of wild animals (Wintle et al., 2020), remarkably deteriorated air quality (Guo et al., 2010; Liu et al., 2018; Marlier et al., 2012; Volkova et al., 2019), severely damaged ecosystems (Cerda et al., 2012), massive economic losses (Stephenson et al., 2013), and regional or global climate change (Abram et al., 2021; Jacobson, 2014; Twohy et al., 2021; Wang et al., 2020).
Due to wildfires' great influences, growing emphasis has been placed on the
monitoring of wildfires based on remote sensing products. Since the 1970s, the
implementation of and research into satellite-based fire detection have been in
the USA using National Oceanic and Atmospheric Administration (NOAA) series
satellites (
Thanks to its easy access, long time series and reliable accuracy (Giglio
et al., 2018), the Moderate Resolution Imaging Spectroradiometer (MODIS)
fire product, with a spatial resolution of 1 km and a temporal resolution of
12 h and available since 2000, has become one of the most widely
employed fire products to monitor the temporal evolution of large-scale wildfires, including forest fires (Mohajane et al., 2021), grassland fires
(Zhang et al., 2017) and crop residue burning (Li et al., 2016). With a
similar temporal resolution (12 h), the Visible Infrared Imaging
Radiometer Suite (VIIRS) fire products with a spatial resolution of 375 m have
been available for fire detection since 2011. Despite a higher spatial
resolution, VIIRS fire products are produced using fewer bands than MODIS
fire products, and the mainly used 4
In recent years, with the growing need for real-time monitoring of a diversity of environmental issues and ecological processes, some satellites have been launched to provide remote sensing products with extremely high temporal resolution. GEOS-16 Advanced Baseline Imager (ABI) active fire products, with a temporal resolution of 5 min and a spatial resolution of 2 km, have been available since 2017 (Hall et al., 2019). GEOS-ABI fire products can effectively monitor medium- to large-scale fires and be used for estimating fire emissions. GEOS-ABI fire products may lead to a poor detection accuracy when identifying small-scale fires (Li et al., 2020). GEOS-ABI mainly provides regional fire products in the southeastern conterminous United States (CONUS). Himawari-8 products, with a spatial resolution of 2 km and temporal resolution of 10 min, have been widely employed to monitor meteorology and wildfires in Asia and Australia since 2015 (Xu et al., 2017). Similarly to GEOS-16 ABI fire products, Himawari-8 fire products are also limited in effectively detecting small-scale fires (Wickramasinghe et al., 2018). Despite an extremely high temporal resolution, fire products produced using geostationary satellites only cover a regional area and cannot monitor the distribution and evolution of wildfires at a global scale.
Long-term running leads to the aging of sensors (Sayer et al., 2015; Liu et al., 2017; Barnes et al., 2019) and causes the degradation of sensor sensitivities (Lyapustin et al., 2014; Doelling et al., 2015; Xiong et al., 2019), increased system errors (Fensholt and Proud, 2012; Xie et al., 2011) and decreased product quality (Fang et al., 2012; Wang et al., 2012). With a high temporal resolution and so far the longest time series, MODIS global fire products have become the most important data source for examining historical regional and global fires, monitoring occurring fires, and investigating their environmental influences. However, after 22 years of running, the gradual aging of sensors will cause, if it has not already, the degradation of MODIS global fire products. To continuously make full use of the existing long-term series of MODIS fire products, even if MODIS degrades or stops services in the future, a fire product with good reliability, good consistence and similar characteristics is urgently needed to serve as a potential alternative to and continuity for global MODIS fire products. Since the launch of the Fengyun-3C (FY-3C) satellite in September 2013, a series of FY meteorological satellites have been designed to produce global active fire products. FY-3C Visible and Infrared Radiometer (VIRR) fire products were produced based on an effective active fire detection algorithm (Lin et al., 2017), which considered dynamic thresholds and infrared gradients. However, the overall accuracy of FY-3C VIRR fire products remained unsatisfactory at the global scale and have thus not been publicly released.
In November 2017, the Fengyun-3D (FY-3D) satellite was launched with an
improved Medium Resolution Spectral Imager (MERSI) for fire detection. With
a similar spatiotemporal resolution, FY-3D provides a promising solution for
the continuity of global MODIS fire products. In this paper, we introduce
the characteristics and fire detection algorithms of a new global fire
product based on FY-3D (recently downloadable from our official website
As one of the core instruments of the Fengyun-3 (FY-3) satellites, the updated Medium Resolution Spectral Imager (MERSI) has become one of the most advanced remote sensing instruments based on wide-swath imaging. The FY-3D satellite was launched in November 2017 with 10 sets of remote sensing instruments, including the Medium Resolution Spectral Imager II (MERSI-II). MERSI-II integrates the functions of the two original imaging instruments (MERSI-I and VIRR) of FY-3B and FY-3C, with a total of 25 channels, including visible light, near infrared, medium infrared and far infrared (as in Table 1). The infrared imaging, detection sensitivity and calibration accuracy of MERSI-II are improved greatly. It is the first imaging instrument that can access the 250 m resolution infrared split-window area globally and capture seamless 250 m resolution true-color global images on a daily basis. MERSI-II also enables the high-quality retrieval of atmospheric, land and marine parameters such as clouds, aerosols, vapor, land surface features and ocean color, supporting global support for environment and climate issues.
Major channel parameters of FY-3D MERSI-II (compared with MODIS/Aqua).
There are two middle-infrared bands (3.8 and 4.05
MERSI-II fire monitoring products from the FY-3D satellite can provide fire spot
location, sub-pixel fire spot area, temperature and fire spot intensity in
inland areas around the world and generate global fire spot pixel
information (including day and night) in HDF files. FY-3D fire products
are produced following a projection with equal latitude and longitude
(0.01
The algorithm for fire spot identification depends on the sensitivity of mid-infrared channels to high-temperature heat sources. The radiance and brightness temperature of the pixels in the mid-infrared channels with sub-pixel fire spots are higher than those of the surrounding non-fire pixels and those of the pixels in the far-infrared channels. Therefore, the pixels with fire spots can be identified by setting an appropriate threshold, and the estimation of background temperature is the key to high detection accuracy and sensitivity.
Sub-pixel fire spot estimation relies on the brightness temperature in mid-infrared channels, and the far-infrared channels are employed when the mid-infrared channels have saturated brightness temperature. In the single-channel estimation formula, the temperature of the open-flame spot is set to 750 K.
Fire spot intensity, namely fire radiation power (FRP), is obtained by
substituting the area and temperature of sub-pixel fire spots into the
Stefan–Boltzmann formula of full-band blackbody radiation.
FRP is divided into 10 levels, indicating different ranges of radiation intensity and the fire behavior at fire spot pixels. Fire spots are classified into four groups with regard to credibility, namely the real fire spots, possible fire spots, fire spots affected by the cloud and noisy fire spots (disturbed by clouds and noise).
FY-3D MERSI-II daily global fire monitoring products are illustrated in Fig. 1. The major processing of daily fire spot products is the generation of 5 min fire spot lists, which include such information as the observation time of fire spot pixels, latitude and longitude, the sub-pixel fire spot area and temperature, and FRP. Next, all the 5 min fire spot information for each day is merged into the daily global fire information list.
FY-3D MERSI-II monthly global fire monitoring products consist of the
information list of global fire spot pixels and the density map of global
fire spots. The information list of monthly global fire spots covers all
global fire spot pixels in the particular month. Concerning the multi-time monitoring
information of the same pixel, the maximum fire spot area is taken as the
current-month fire spot information for the pixel. Figure 2 is an illustration
of the density map of global fire spots based on FY-3D MERSI-II, in which
different colors indicate the number of fire spot pixels on a 0.25
Thematic map of global fire monitoring by FY-3D (13 June 2019). The
color bar with different colors means the number of fire spots in the
0.25
Density map of global fire spots based on FY-3D (June 2019). Fire-prone areas were distributed in northern Russia, south-central Africa, southeastern South America, the coastland of Australia and small parts of Canada.
This section mainly introduces the specific algorithm and steps for generating FY-3D global fire products based on the original data obtained from MERSI-II. The input data include MERSI-II global orbital Earth observations, MERSI-II global orbital geographical locations, MERSI-II global orbital cloud detection data, and global land and sea template data, as shown in Table 2.
Input file list of MERSI-II global fire monitoring software.
Automatic identification of fire spots is the major step for generating fire
products. Firstly, the 5 min level-1 (L1) data segments of MERSI-II and various
auxiliary data are read in, and the noise lines are identified to generate
the noise line mark. Next, the 5 min data segments are projected
according to the rule of the equal latitude and longitude and cut as
5
General flowchart for generating FY-3D MERSI-II fire spot products.
Channel 20 of FY-3D MERSI-II is mid-infrared, with a wavelength of
3.55–3.95
As indicated by Fig. 4a, when the fire spot temperature grows, the brightness temperature of Channel 20 (CH20) pixels increases rapidly. Even if the fire spot only accounts for 0.1 % the pixel area, the brightness temperature increment can reach 10 K (44 K) when the fire spot is 500 K (900 K). Although the brightness temperature increase of CH24 also rises with the higher fire spot temperature, it is far lower than that of CH20. Figure 4b illustrates that as the fire spot area becomes larger, the brightness temperature of CH20 mixed pixels grows rapidly. It reaches 12 K when the fire spot is 900 K, even if the fire spot only accounts for 0.01 % of the pixel area. Similarly, the brightness temperature increment of CH24 grows at a much lower rate than that of CH20.
Effective cloud detection is required for generating reliable fire products for the following reasons. Firstly, the existence of cloud in the atmospheric layers may block the emitted information of fire spots, leading to missed identification. Secondly, specular reflection of cloud can lead to wrong identification of fire spots. Therefore, cloud identification was conducted before fire identification. Similarly to MODIS, FY-3D also included radiation information from multiple bands, and the principle of cloud identification for FY-3D fire products was similar to that of MODIS. Based on the reflectance difference between cloud and land pixels, we classified cloud pixels following the rules listed in Table 3.
Major rules for cloud pixel identification.
According to the principle of fire spot identification, when a fire spot appears in a pixel (i.e., open flame), the brightness temperature of the pixel in Channel 20 is significantly higher than the background brightness temperature (the brightness temperature of surrounding non-fire pixels); the brightness temperatures of Channels 24 and 25 are also higher than the background, but the temperature difference is much smaller than that of Channel 20. In this case, the difference in brightness temperature between fire spot pixels and background in both the mid-infrared channel and far-infrared channels can be employed as important factors for automatic identification of fire spots. Therefore, the background temperature of the detected pixel is required for identifying fire spots. Since the background temperature cannot be obtained from the fire spot pixels, it should be calculated according to the average of their surrounding pixels. However, the reflection of solar radiation during the daytime also causes a higher brightness temperature in the mid-infrared channel, which mainly occurs in the zone bare of vegetation, cloud surface and water bodies (specular reflection). In particular, the difference in brightness temperature between mid-infrared and far-infrared channels caused by specular reflection of solar radiation can reach tens of kelvins on the cloud surface and water bodies. Since the reflection of solar radiation on the bare surface is relatively weak in the mid-infrared channel, a few degrees of difference can cause non-fire pixels misclassified as fire pixels due to the high sensitivity requirement for fire identification. When the background brightness temperature is calculated, pixels that already contain fire spots should also be excluded. Therefore, suspected high-temperature pixels, which may already contain fire spot pixels, cloudy pixels, water pixels and those pixels affected by solar flare, should be removed for background temperature calculation.
Furthermore, the pixel size in the mid-infrared channel of a meteorological
satellite is about 1 km
After the abovementioned disturbing pixels were removed, the average and standard deviation of background temperature in the mid-infrared channel and the background average and standard deviation of brightness temperature difference between the mid-infrared and far-infrared channels were calculated with peripheral pixels as background pixels.
The calculation of background temperature was acquired in the following
steps. For each
With obtained background temperature, the difference between brightness temperature and background temperature in the mid-infrared channel, as well as the difference in brightness temperature and background temperature between mid-infrared and far-infrared channels, at the candidate pixels could be calculated, based on which we could decide whether the threshold of fire spot identification was reached. If the threshold was reached, the pixel is preliminarily marked as a fire pixel. Next, for daytime observation data, it is necessary to further check whether the increase in brightness temperature in the mid-infrared channel was interfered with by solar radiation in the cloud area. Through the two-stage check, fire pixels could be effectively extracted.
When the following two conditions are met, a pixel can be identified as a fire
pixel:
Here
Satellite data received by the ground system contain noise. For instance, some scanning lines may contain many noisy pixels that affect fire spot identification. In this case, noise lines, referred to multiple consecutive noisy pixels in one scanning line, should firstly be checked. Since the identification of fire was carried out on the areal map projected with an equal latitude and on the same circle of longitude, the identified latitude and longitude of fire spots failed to reflect the original positions of scanning lines. Therefore, the noise line was identified on the 5 min data segments before projection. Firstly, the 5 min data segments were employed to identify fire spots, and the line number of identified fire spot pixels was recorded. Following this, the number of fire spot pixels in each line was counted. When the number of fire spot pixels in a line exceeded the empirical threshold, it was identified as a noise line and all pixels in the line are marked as noisy ones. In the following process, all pixels in this line were no longer considered for fire spot identification.
FRP can be calculated using the Stefan–Boltzmann formula (Matson and Schneider, 1984) through the estimation of the sub-pixel fire spot area and temperature.
MERSI-II data are 12 bit, with a quantization level of 0–4095 and high
radiation resolution. The spatial resolution is 1.1 km, and the radiance of
a pixel observed by the satellite is the weighted average of the radiance of
all the ground objects within the pixel range as
Due to different FRP levels and temperatures, underlying surfaces containing fire
spots can be divided into fire zones and non-fire zones (background). When
fire spots appear, the radiance of pixels containing fire spots (i.e., mixed
pixels) can be expressed by the following formula:
For Eq. (4), there are two unknown variables,
When a single channel was adopted to estimate the sub-pixel fire spot area, the fire spot temperature was set to an appropriate value, which was 750 K in this product.
Based on the percentage of the sub-pixel fire spot area,
Wildfires are characterized by random and rapid changes, so it is difficult to verify the product accuracy of GFR (global fire) according to actual ground information. In this paper, the accuracy of FY-3 fire products is tested through visual interpretation and cross-verification of other products. Specifically, due to the extremely large size of GFR datasets, we set the different strategies for accuracy assessment. For visual interpretation, several 5 min data segments with regional representation were selected for verification using manually identified fire spots. For cross-verification with other fire products, global fire spot data throughout 2019 were employed.
The error was defined as the distance from the positions (longitude and
latitude) of automatically identified fire spot pixels to corresponding
manually identified ones. When the difference in latitude and longitude was
less than or equal to 0.02
In addition to the visual-check-based accuracy assessment at the global scale, we also employed a set of field-collected reference data to verify the suitability of FY-3D in China, which is further explained in the following sections.
In this research, 5 min segments of FY-3D fire products in different continents, including Africa, South America, the Indochinese Peninsula, Siberia and Australia, were collected at 12:15 (UTC) on 13 June 2018, 17:05 (UTC) on 21 August 2019, 06:15 (UTC) on 13 March 2019, 03:40 (UTC) on 13 November 2019 and 17:40 (UTC) on 29 May 2018, respectively, for visual interpretation. The specific observation positions are shown in Fig. 5 with five corresponding fire detection pictures of FY-3D.
These regions were selected for evaluating the global reliability of FY-3D fire products for the following reasons. Firstly, Africa, South America, the Indochinese Peninsula, Siberia and Australia are the regions with the most frequent fire events across the globe. Secondly, there is rich vegetation in these regions, which provides the foundation for stable combustion across a year. Thirdly, these regions cover large areas with generally unified underlying surfaces. Fourthly, these areas are of regional representation: Siberia represents typical regions with frequent forest fires in the Northern Hemisphere. Africa represents typical tropical grasslands and forests in the Equator regions. South America represents virgin tropical rain forests.
Figure 5 presents the spatial distribution of GFR spots and manually identified fire pixels in the 5 min segment of the above regions. According to Fig. 5b, most fire spots in FY-3D products and manually extracted fire spots in South America were in the same positions. In Fig. 5c, most FY-3D and manually extracted fire spots in Africa coincided or were in a close position. In Fig. 5d, despite a few mismatched fire spots, the positions of FY-3D and manually extracted fire spots in the Indochinese Peninsula were consistent. Figure 5e and f also show that most fire spots are matched in Russia and Australia. Table 4 shows accuracy of GFR spots in the five typical regions. The accuracy of automatically identified fire spot in all regions was generally consistent and all exceeded 90 %. Since these selected regions represented distinct vegetation types and are located in different hemispheres, the verification of FY-3D fire products based on 0.24 SMART proved its stability and reliable high-accuracy at the global scale.
It is worth mentioning that the visual-check-based accuracy assessment
mainly considered the commission error, while omission error cannot be
effectively revealed for the following reason. The omitted fires were mainly
caused by the requirement of a minimum burning area. Since the spatial
resolution of FY-3D and MODIS active fire products is 1 km, small fires (less
than 100 m
The cross-verification between FY-3D fire products and the mainstream MODIS
fire products, MYD14A1 V6 (
Accuracy assessment of FY-3D-identified fires based on SMART (visual check).
The consistence between FY-3D and MODIS fire products in different months (2019).
In addition to the overall consistence between MODIS and FY-3D fire products, we also conducted cross-verification between the two global fire products in different months, underlying surfaces, regions and fire intensities as follows.
Figure 7a illustrates the monthly consistence between FY-3D and MODIS fire products in 2019. The consistence in the remaining months is over 80 % except in April, October and November. The highest appears in July, exceeding 90 %, while the lowest is in April, at 71 %. Detailed parameters can be found in Table 5. From a global perspective, the number of fire spots was larger in July, August and September and the mean consistence between MODIS and FY-3D fire products was larger than 85 %. For July when the fire products were the most numerous, the consistence achieved 90 %. From January to May, the number of fire spots was relatively small, and the mean consistence was around 80 %. The consistence for April was 71 %, the lowest among all months. The notable monthly variations in the consistence between MODIS and FY-3D fire products was mainly attributed to the uneven spatial distribution of fire spots across the globe. As shown in Fig. 6, in June and July, a large number of fire spots were mainly concentrated in Africa, South America and Eurasia, leading to a high consistence of fire identification. In April, there were limited and sparsely distributed fire spots in Africa and South America, leading to a low consistence. According to the statistics, the number of fire spots was positively correlated with the consistence between different fire products. Meanwhile, in seasons when fire could last longer, the consistence was higher.
Cross-satellite comparison between FY-3D and MODIS fire products.
Statistical analysis of consistence is carried out with different types of underlying surface. The data of underlying surfaces are according to the global land use detailed in Table 6.
The 15 types of underlying surfaces were selected for verification. Table 6
and Fig. 7c show the consistence of FY-3D and MODIS fire products with
different underlying surfaces. From the classification of different
underlying surfaces, the remaining types are over 80 % consistent except (11) Post-flooding or irrigated croplands (or aquatic), (14) Rainfed crops, (20) Mosaic cropland (50 %–70 %)/vegetation (grassland/shrubland/forest)
(20 %–50 %), (140) Closed to open (
The low consistence between FY-3D and MODIS fire products was observed for underlying surfaces 11, 14, 20, 140 and 150. Specifically, 11, 14 and 20 could be categorized as farmlands. Surface 140 was mainly occupied by herbaceous vegetation or sparse grasslands. Surface 150 was mainly occupied by sparse grasslands. Generally, these surfaces were all covered by sparse or unstable vegetation, on which the fire can last for a relatively short period. Meanwhile, the observation time lag between FY-3D and MODIS was larger than 30 min. Therefore, the consistence of FY-3D and MODIS fire products on these surface types was lower than on other surface types.
Classification of underlying surfaces (land cover types).
The consistence between FY-3D and MODIS fire spots on different underlying surfaces in each month (total FY-3D pixels(consistence)).
The global monitoring area is divided into Africa, America, Asia, Europe and Oceania. The verification demonstrates the results with the highest consistence (over 80 %) are found in Africa and Asia, and those in America, Europe and Oceania show consistence over 70 %. The FY-3D MERSI-II fire identification algorithm draws lessons from the MODIS algorithm and has been improved on that basis, and targeted development has been made for the underlying surface and climatic conditions in China, so it is necessary to test the matching results in China separately. This shows that China's regional consistence of results is lower than for other continents, at only 65 %. To further examine the suitability of FY-3D fire products in China, an accuracy assessment of FY-3D and MODIS fire products was conducted based on ground truth data and is explained in the following sections.
Consistence between FY-3D and MODIS fire products under different
conditions.
The confidence of fire spots and the fire intensity represented by FRP are analyzed, and the data come from the MODIS fire spot list. Figure 8a and b are statistical diagrams of confidence and FRP, respectively. From Fig. 8a, the confidence of the matched pixels of the two satellites is above 66 %, while that of the mismatched ones is less than 60 % and even lower than 50 % in some months. In other words, the higher confidence indicates the higher matching degree. As indicated by Fig. 8b, the FRP of the matched pixels of two satellites is mostly above 40 MW, while that of the unmatched pixels is less than 40 MW and even lower than 20 MW in some months. Accordingly, the greater fire intensity leads to a greater probability of simultaneous observation by the two satellites and a higher matching degree between their results.
Two major findings were identified based on the comparison between FY-3D and MODIS fire products in terms of fire intensity: firstly, the higher the credential of the identified fire, the higher consistence between FY-3D and MODIS fire products. When the credential was larger than 65 %, both FY-3D and MODIS could effectively identify the candidate pixel as a fire pixel. In other words, the parameter of credentials in the MODIS fire product provides an important reference for fire detection. Secondly, FRP is an index for the heat radiation of the fire. The larger the FRP, the larger the consistence between FY-3D and MODIS, indicating a higher accuracy of fire detection. Therefore, the difficulty for fire detection mainly lies in the detection of weak fires.
In addition to visual check and consistence check, we also referred to a large-scale field experiment to comprehensively assess the suitability of FY-3D fire products in China. The State Grid Corporation of China and China Meteorological Administration jointly conducted a fire detection experiment throughout 2020 in five provinces in China: Guangdong, Guangxi, Yunnan, Guizhou and Hainan. This experiment was conducted in the following steps. A large number of drones were employed to check the occurrence of fires. According to the local passing time of FY-3D, these drones reported the coordinates of actual fires for verifying the accuracy of FY-3D-identified fires. The temporal difference between the passing time of FY-3D and reported time was controlled to within 1 h. In this way, both omitted and misidentified fires could be effectively recognized (as shown in Fig. 9). Based on the field-collected reference of fires, we evaluated the suitability of FY-3D fire products in China (Table 8).
Accuracy assessment of FY-3D fire products in China based on the ground-based reference.
Accuracy assessment based on field ground truth.
As shown in Fig. 9 and Table 8, FY-3D products achieved a good accuracy of 79.43 % in China. Meanwhile, MODIS also achieved a good accuracy of 74.23 %. As introduced above, the omission error in FY-3D and MODIS fire products was mainly attributed to a small fire area, which failed to meet the minimum fire area recognizable by sensors. When simply considering the commission error, FY-3D fire products achieved an accuracy of 88.50 %, notably higher than that of MODIS (79.69 %). This result proved that with the consideration of local underlying surfaces, FY-3D fire products are more suitable for fire monitoring in China.
As satellite instruments keep aging in the harsh space environment, the degradation of sensors is inevitable (Tian et al., 2015). Theoretically, sensor degradation can be corrected through atmospheric calibration. However, during the mission life, the solar diffuser and stability monitor required for atmospheric calibration also change across time (Wang et al., 2012). Since the MODIS instrument has been working for more than 20 years, its performance for fire detection will degrade, if it has not already, in the future. Furthermore, similarly to VIIRS and other algorithms, MODIS fire products may have large uncertainties in such regions as China (Fu et al., 2020; Ying et al., 2019). As major products of the FY-3D meteorological satellite, FY-3D fire products boast a high resolution and accuracy in China by specifically including the underlying surface parameters collected in China. Compared with MODIS and VIIRS, MERSI-II shows a resolution of 250 m in the far-infrared channel, which is the highest among meteorological satellites of the same type. The FY-3D fire identification algorithm learns from the advantages and technical ideas of MODIS and VIIRS fire identification algorithms. Furthermore, FY-3D fire products have been optimized in terms of auxiliary parameters, fire identification and re-identification as follows.
The MODIS fire product is one of the most significant and frequently employed fire products with mature algorithms. Compared with MODIS, FY-3D receives limited emphasis for its capability for fire monitoring, which is mainly attributed to its short service periods. On one hand, due to its long time series and general reliability, MODIS fire products have remained a popular choice for monitoring long-term variations in fire spots across the world. However, the long-term running of MODIS sensors has led to growing uncertainties about the quality of recent and future MODIS fire products. In this regard, thanks to its similar spatiotemporal resolution, high consistence and visiting time difference of less than 1 h, FY-3D fire products have the potential to be widely employed as a potential alternative to and continuity for global MODIS fire products. Meanwhile, FY-3D fire products have a higher reliability in China and its surrounding regions than other fire products. Therefore, FY-3D fire products are an ideal selection for fire monitoring in China.
The main implementation of FY-3D fire products is fire monitoring. For vast
forest and grassland areas, it is inefficient and time-consuming for manual
and aircraft patrols to monitor wildfires. Satellite remote sensing can work
for a continuous space with a wide monitoring range, providing massive amounts of
information in fire detection, disaster relief and post-disaster
assessment. In addition to fire spot identification and real-time fire
tracking, the impact of pollutants produced by biomass combustion on the
environment is another important topic. In China and Southeast Asia, air
pollution caused by biomass burning has intensified in recent years.
Agricultural activities such as crop residue burning and wildfires (e.g., forest fires and grassland fires) emit airborne pollutants (e.g., PM
China recently launched the FY-3E and FY-4B satellites in June and July 2021. Amid the launch and operation of a new generation of Fengyun meteorological satellites, the accuracy and timeliness of fire monitoring by meteorological satellites have been largely enhanced. Thanks to improved meteorological data, which provide a useful reference to understand the current status of combustibles and potential fire risk, the FY-3D satellite will be taken as a better data source to produce various secondary products for fire monitoring and prediction. Based on traditional fire spot identification, further research should concentrate on the assessment of the fire area, estimation of biomass carbon emissions, prediction of smoke impact, and early warning of forest and grassland fire using the series of Fengyun meteorological satellites. For instance, the water content of combustibles is closely related to temperature, light and cloud cover, which are important indicators in forest and grassland fire forecasts. However, this variable has rarely been considered in previous fire products. Based on a series of products from Fengyun meteorological satellites, such as the surface temperature, vegetation index, surface evapotranspiration, solar radiance and cloud cover, FY-3D fire products can be improved by establishing an estimation model for the water content of combustibles. Meanwhile, with fire products such as fire spots and smoke and meteorological products such as wind field data from Fengyun series satellites, we can predict the impact of smoke caused by forest and grassland fires on the atmospheric environment in the surrounding areas. In future implementations, Fengyun meteorological satellites will play a greater role in monitoring, forecasting and early warning of global fires and their ecological impacts.
MYD14A1 Version 6 is available via the NASA FIRMS portal (
With a similar spatial and temporal resolution, we produced FY-3D global fire products, aiming to serve as a potential alternative to and continuity for MODIS fire products. The sensor parameters and major algorithms for noise detection and fire identification in FY-3D products were introduced. For visual-check-based accuracy assessment, five typical regions across the globe, Africa, South America, the Indochinese Peninsula, Siberia and Australia, were selected, and the overall accuracy exceeded 94 %. We also compared the FY-3D and MODIS fire products for their consistence. The result suggested that the overall consistence was 84.4 %, with fluctuation across seasons, surface types and regions. The high accuracy and consistence with MODIS products proved that the FY-3D fire product is an ideal tool for global fire monitoring. Based on field-collected reference data, we further evaluated the suitability of FY-3D fire products in China. The overall accuracy and accuracy without considering omission errors were 79.43 % and 88.50 % higher, respectively, than those of MODIS fire products. Since detailed geographical conditions in China were considered, FY-3D products should be preferably employed for monitoring fires and estimating their environmental effects in China.
JC, WZ and CL produced FY-3D global fire products and the official website. JC, ZC, BG and ML conceived the manuscript. JC, CZ, QY, MX, XC and JY conducted data analysis and produced figures. JC and ZC wrote the draft. ZC and ML reviewed and revised the manuscript.
The contact author has declared that neither they nor their co-authors have any competing interests.
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Thanks to the two anonymous reviewers for the valuable comments. This research is supported by the National Natural Science Foundation of China (grant no. 42171399) and the National Key Research and Development Program of China (grant no. 2021YFC3000300).
This research has been supported by the National Natural Science Foundation of China (grant no. 42171399) and the National Key Research and Development Program of China (grant no. 2021YFC3000300).
This paper was edited by Bo Zheng and reviewed by two anonymous referees.