Investigations on Land and Forest Fires in the North Indian Region over a Decade

2021 ◽  
pp. 105-115
Author(s):  
Narendra Singh ◽  
Ashish Kumar
Keyword(s):  
Forest Fires ◽  
Indian Region ◽  
The North

scholarly journals Estimation of emissions from biomass burning in China (2003–2017) based on MODIS fire radiative energy data

2019 ◽  
Vol 16 (7) ◽  
pp. 1629-1640 ◽  
Author(s):  
Lifei Yin ◽  
Pin Du ◽  
Minsi Zhang ◽  
Mingxu Liu ◽  
Tingting Xu ◽  
...  
Keyword(s):  
Biomass Burning ◽  
Forest Fires ◽  
Crop Residue ◽  
Crop Yields ◽  
Southern China ◽  
Farming System ◽  
Radiative Energy ◽  
Fire Emissions ◽  
The North ◽  
Significant Downward Trend

Abstract. Biomass burning plays a significant role in air pollution and climate change. In this study, we used a method based on fire radiative energy (FRE) to develop a biomass burning emission inventory for China from 2003 to 2017. Daily fire radiative power (FRP) data derived from 1 km MODIS Thermal Anomalies/Fire products (MOD14/MYD14) were used to calculate FRE and combusted biomass. Available emission factors were assigned to four biomass burning types: forest, cropland, grassland, and shrubland fires. The farming system and crop types in different temperate zones were taken into account in this research. Compared with traditional methods, the FRE method was found to provide a more reasonable estimate of emissions from small fires. The estimated average annual emission ranges, with a 90 % confidence interval, were 91.4 (72.7–108.8) Tg CO2 yr−1, 5.0 (2.3–7.8)  Tg CO yr−1, 0.24 (0.05–0.48) Tg CH4 yr−1, 1.43 (0.53–2.35) Tg NMHC yr−1, 0.23 (0.05–0.45) Tg NOx yr−1, 0.09 (0.02–0.17) Tg NH3 yr−1, 0.03 (0.01–0.05) Tg SO2 yr−1, 0.04 (0.01–0.08) Tg BC yr−1, 0.27 (0.07–0.49) Tg OC yr−1, 0.51 (0.19–0.84) Tg PM2.5 yr−1, 0.57 (0.15–1.05) Tg PM10 yr−1, where NMHC, BC, and OC are nonmethane hydrocarbons, black carbon, and organic carbon, respectively. Forest fires are determined to be the primary contributor to open fire emissions, accounting for 45 % of the total CO2 emissions (average 40.8 Tg yr−1). Crop residue burning ranked second place with a large portion of 39 % (average 35.3 Tg yr−1). During the study period, emissions from forest and grassland fires showed a significant downward trend. Crop residue emissions continued to rise during 2003–2015 but dropped by 42 % in 2015–2016. Emissions from shrubland were negligible and little changed. Forest and grassland fires are concentrated in northeastern China and southern China, especially in the dry season (from October to March of the following year). Plain areas with high crop yields, such as the North China Plain, experienced high agricultural fire emissions in harvest seasons. Most shrubland fires were located in Yunnan and Guangdong provinces. The resolution of our inventory (daily, 1 km) is much higher than previous inventories, such as GFED4s and GFASv1.0. It could be used in global and regional air quality modeling.

scholarly journals Spatial Distribution of Atmospheric Aerosol Physicochemical Characteristics in the Russian Sector of the Arctic Ocean

Atmosphere ◽  
2020 ◽  
Vol 11 (11) ◽  
pp. 1170
Author(s):  
Sergey Sakerin ◽  
Dmitry Kabanov ◽  
Valery Makarov ◽  
Viktor Pol’kin ◽  
Svetlana Popova ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
Chemical Composition ◽  
Arctic Ocean ◽  
Black Carbon ◽  
Forest Fires ◽  
Barents Sea ◽  
The Arctic ◽  
The North ◽  
The Barents Sea ◽  
The Arctic Ocean

The results from studies of aerosol in the Arctic atmosphere are presented: the aerosol optical depth (AOD), the concentrations of aerosol and black carbon, as well as the chemical composition of the aerosol. The average aerosol characteristics, measured during nine expeditions (2007–2018) in the Eurasian sector of the Arctic Ocean, had been 0.068 for AOD (0.5 µm); 2.95 cm−3 for particle number concentrations; 32.1 ng/m3 for black carbon mass concentrations. Approximately two–fold decrease of the average characteristics in the eastern direction (from the Barents Sea to Chukchi Sea) is revealed in aerosol spatial distribution. The average aerosol characteristics over the Barents Sea decrease in the northern direction: black carbon concentrations by a factor of 1.5; particle concentrations by a factor of 3.7. These features of the spatial distribution are caused mainly by changes in the content of fine aerosol, namely: by outflows of smokes from forest fires and anthropogenic aerosol. We considered separately the measurements of aerosol characteristics during two expeditions in 2019: in the north of the Barents Sea (April) and along the Northern Sea Route (July–September). In the second expedition the average aerosol characteristics turned out to be larger than multiyear values: AOD reached 0.36, particle concentration up to 8.6 cm−3, and black carbon concentration up to 179 ng/m3. The increased aerosol content was affected by frequent outflows of smoke from forest fires. The main (99%) contribution to the elemental composition of aerosol in the study regions was due to Ca, K, Fe, Zn, Br, Ni, Cu, Mn, and Sr. The spatial distribution of the chemical composition of aerosols was analogous to that of microphysical characteristics. The lowest concentrations of organic and elemental carbon (OC, EC) and of most elements are observed in April in the north of the Barents Sea, and the maximal concentrations in Far East seas and in the south of the Barents Sea. The average contents of carbon in aerosol over seas of the Asian sector of the Arctic Ocean are OC = 629 ng/m3, EC = 47 ng/m3.

Soil record of the Holocene paleofires at the north of European Russia

2020 ◽  
Author(s):  
Nikita Mergelov ◽  
Dmitry Petrov ◽  
Andrey Dolgikh ◽  
Elya Zazovskaya
Keyword(s):  
Kola Peninsula ◽  
Forest Fires ◽  
Soil Formation ◽  
Basic Research ◽  
Isotope Ratio Mass Spectrometry ◽  
Local Scale ◽  
14C Dating ◽  
The Holocene ◽  
Arkhangelsk Region ◽  
The North

<p>Soils and sediments serve as complementary sources of detailed information on paleofires in various ecosystems. Despite the abundance of charcoal material entrapped in soils they remain relatively less studied pyrogenic archives in comparison to the sedimentary paleofire records (e.g. lacustrine and peat deposits), and that is especially the case for the most territory of Russia. We report here on the numerous soil archives of the Holocene forest fires at the Kola Peninsula (66.347°N, 37.948°E) and the north of Arkhangelsk region (64.747°N, 43.387°E) in Russia. Series of buried Podzols (up to ten successive profiles) separated by the distinct charcoal layers were revealed in specific geomorphological traps like the thermokarst depressions inherited from the early stages of moraine sediments formation (Kola Peninsula), as well as in active and paleokarst sinkholes in carbonate and sulfate rocks (Arkhangelsk region). The maximum temporal depth of archives was estimated as 10261±40 cal yr BP for the key site in Arkhangelsk region, with up to 12 major pyrogenic events recorded at the local scale. Soil formation at the inter-pyrogenic stages maintained a uniform direction for at least 10 thousand years and profiles of Podzols were regularly replicated at all the key sites. We employ here a combination of soil morphological hierarchical analysis, study of geomorphological processes leading to the burial of pyrogenic carbon, 14C dating of charcoal and TOC derived from the soil organic matter, carbon and nitrogen isotope ratio mass spectrometry and anthracomass concentrations analysis to extract a set of paleoenvironmental information from these soil archives. The study of complementary pyrogenic archives in the three-component system of the karst landscape (including bottom and slopes of the funnels, as well as the flat elevated areas between them) helped to mitigate overestimation or underestimation of the anthracomass concentration and allowed to acquire a detailed dataset on paleopyrogenic events at the local scale. This study is supported by the Russian Foundation for Basic Research, Project No. 19-29-05238.</p>

The late Quaternary geology of the Chalk River region, Ontario and Quebec

1982 ◽  
Vol 19 (6) ◽  
pp. 1218-1231 ◽  
Author(s):  
N. R. Catto ◽  
R. J. Patterson ◽  
W. A. Gorman
Keyword(s):  
Forest Fires ◽  
Late Quaternary ◽  
Glacial Ice ◽  
Ottawa River ◽  
The North ◽  
Discharge Rates ◽  
Aeolian Activity ◽  
River Region ◽  
Ice Retreat ◽  
Time Changes

Glacial ice covered the Chalk River area through most of the Wisconsin Stage. About 11 300 years ago, an ice retreat was followed immediately by a short incursion of Champlain Sea waters, which deposited at least 2.5 m of clay, silt, and sand. A local readvance, probably associated with the St. Narcisse event, deposited till on the marine sediments. Following the final retreat of the ice from the area, lacustrine and aeolian deposition occurred locally for a short time.About 10 500 years ago, the North Bay drainage route opened, greatly increasing the discharge of the Ottawa River. A faint terrace at a present elevation of 209 m probably formed at this time. Changes in the drainage routes of proglacial lakes and in the rate of ice retreat caused a general decrease in discharge rates, and resulted in the formation of pronounced terraces, now at 180, 160, and 129 m, and fainter terraces at 170, 141, and 137 m. By about 5000 years BP, the North Bay outlet closed, and the river fell to approximately 111 m, its present elevation at Chalk River.During the whole period of terrace formation, alluvial sands were being deposited and, as river levels fell, exposed sands were reworked by the wind until anchored by vegetation. Charcoal horizons within the aeolian sequences indicate that forest fires occasionally destroyed the vegetation cover, re-initiating aeolian activity. Locally, active dunes are present near Chalk River, but most of the area has been stabilized by vegetation.

scholarly journals Thunderstorm climatology over Indian region

MAUSAM ◽  
2021 ◽  
Vol 58 (2) ◽  
pp. 189-212
Author(s):  
AJIT TYAGI
Keyword(s):  
West Bengal ◽  
Thunderstorm Activity ◽  
Severe Weather ◽  
Indian Region ◽  
Quality Data ◽  
Full Time ◽  
Climatological Data ◽  
The North ◽  
Annual Frequency ◽  
The Impact

Thunderstorm is a severe weather phenomenon, the impact of which is being increasingly felt by all the sectors of society. In this study attempt has been made to develop thunderstorm climatology over Indian region based on latest representative climatological data. In all, data of 450 observatories comprising of 390 IMD observatories, 50 IAF observatories, six Bangladesh observatories, two Pakistan observatories, and one each in Nepal and Sri Lanka have been analysed. Inclusion of climatological data of Indian Air Force and Bangladesh has helped in developing representative climatology over Indian region. The study has brought out higher (100-120 days) annual frequency of thunderstorm as compared to those given by earlier studies (80-100 days). The highest annual frequency (100-120 days) is observed over Assam and Sub Himalayan West Bengal in the east and Jammu region in the north. The lowest frequency (less than 5 days) is observed over Ladakh region. In the plains Gangetic West Bengal and Bangladesh record between 80 and 100 days of thunderstorm annually. Kerala records highest (80-100 days) thunderstorm frequency of thunderstorm over peninsula. Udhampur observatory (132 days) in Jammu sub-division records highest number of thunderstorms in the country followed by Kumbhigram (Silchar) observatory (129 days) in south Assam and Hasimara (123 days) in Sub Himalayan West Bengal. In the plains Saurashtra and Kutch record lowest number (less than 15 days) of thunderstorm in the country. Thunderstorms are primarily short lived mesoscale weather phenomena. Existing synoptic network of part time observatories have limitations in recording all the occurrences of thunderstorms at the observatory and adjoining areas. Inclusion of data from such observatories results in lower frequency of the event and vitiates climatology. Efforts have been made in this study to develop thunderstorm climatology by using quality data of full time current weather (Airport) observatories, class I and selected class II IMD observatories. Since number of full time observatories in most of the sub divisions is few, the study is not able to bring out finer spatial variation of thunderstorm activity with in sub-divisions. Thunderstorm is a high impact severe weather event, which affects all the sectors of the society. Therefore, both from operational and climatological point of view, there is urgent need to establish at least one full time current weather observatory in each district to ensure proper reporting of all thunderstorm occurrences and to build district level thunderstorm climatology in the country.

Effects of Forest Fires on Archaeological Resources at Grand Canyon National Park

1987 ◽  
Vol 7 (3) ◽  
pp. 243-254 ◽  
Author(s):  
Anne Trinkle Jones ◽  
Robert C. Euler
Keyword(s):  
Forest Fires ◽  
Fire History ◽  
Prescribed Burning ◽  
Grand Canyon ◽  
Cultural Resources ◽  
Experimental Conditions ◽  
The North ◽  
Before And After ◽  
History Of ◽  
Fire Area

For a number of years archaeologists have discussed the effects of forest fires on archaeological resources. Studies under experimental conditions and of sites after they were burned form the bulk of this effort but, for the most part, they have not been published. This article examines the fire history of the North Rim of the Grand Canyon and the effects of the Dutton Point wildfire on prehistoric architecture and artifacts—particularly ceramics. Armed with those data, a modest experiment useful in any proposed prescribed fire area containing cultural resources, was designed. This involved “before and after” studies of a ruin that was to be subjected to prescribed burning and included buried temperature controls and the varying effects upon the resource. Finally, a hypothesis regarding the effect of wildfires on archaeological sites is presented.

scholarly journals Uplifting of carbon monoxide from biomass burning and anthropogenic sources to the free troposphere in East Asia

2015 ◽  
Vol 15 (5) ◽  
pp. 2843-2866 ◽  
Author(s):  
K. Ding ◽  
J. Liu ◽  
A. Ding ◽  
Q. Liu ◽  
T. L. Zhao ◽  
...  
Keyword(s):  
East Asia ◽  
Forest Fires ◽  
North China Plain ◽  
North China ◽  
Anthropogenic Sources ◽  
Free Troposphere ◽  
Transport Pathways ◽  
Upper Troposphere ◽  
The North ◽  
The North China Plain

Abstract. East Asia has experienced rapid development with increasing carbon monoxide (CO) emission in the past decades. Therefore, uplifting CO from the boundary layer to the free troposphere in East Asia can have great implications on regional air quality around the world. It can also influence global climate due to the longer lifetime of CO at higher altitudes. In this study, three cases of high CO episodes in the East China Sea and the Sea of Japan from 2003 to 2005 are examined with spaceborne Measurements of Pollution in the Troposphere (MOPITT) data, in combination with aircraft measurements from the Measurement of Ozone and Water Vapor by Airbus In-Service Aircraft (MOZAIC) program. High CO abundances of 300–550 ppbv are observed in MOZAIC data in the free troposphere during these episodes. These are among the highest CO abundances documented at these altitudes. On average, such episodes with CO over 400 ppbv (in the 2003 and 2004 cases) and between 200 and 300 ppbv (in the 2005 case) may occur 2–5 and 10–20% in time, respectively, in the respective altitudes over the region. Correspondingly, elevated CO is shown in MOPITT daytime data in the middle to upper troposphere in the 2003 case, in the lower to middle troposphere in the 2004 case, and in the upper troposphere in the 2005 case. Through analyses of the simulations from a chemical transport model GEOS-Chem and a trajectory dispersion model FLEXPART, we found different CO signatures in the elevated CO and distinct transport pathways and mechanisms for these cases. In the 2003 case, emissions from large forest fires near Lake Baikal dominated the elevated CO, which had been rapidly transported upward by a frontal system from the fire plumes. In the 2004 case, anthropogenic CO from the North China Plain experienced frontal lifting and mostly reached ~ 700 hPa near the East China Sea, while CO from biomass burning over Indochina experienced orographic lifting, lee-side-trough-induced convection, and frontal lifting through two separate transport pathways, leading to two distinct CO enhancements around 700 and 300 hPa. In the 2005 case, the observed CO of ~ 300 ppbv around 300 hPa originated from anthropogenic sources over the Sichuan Basin and the North China Plain and from forest fires over Indochina. The high CO was transported to such altitudes through strong frontal lifting, interacting with convection and orographic lifting. These cases show that topography affects vertical transport of CO in East Asia via different ways, including orographic uplifting over the Hengduan Mountains, assisting frontal lifting in the North China Plain, and facilitating convection in the Sichuan Basin. In particular, topography-induced lee-side troughs over Indochina led to strong convection that assisted CO uplifting to the upper troposphere. This study shows that the new daytime MOPITT near-infrared (NIR) and thermal-infrared (TIR) data (version 5 or above) have enhanced vertical sensitivity in the free troposphere and may help qualitative diagnosis of vertical transport processes in East Asia.

scholarly journals Effects of the 2006 El Niño on tropospheric ozone and carbon monoxide: implications for dynamics and biomass burning

2009 ◽  
Vol 9 (13) ◽  
pp. 4239-4249 ◽  
Author(s):  
S. Chandra ◽  
J. R. Ziemke ◽  
B. N. Duncan ◽  
T. L. Diehl ◽  
N. J. Livesey ◽  
...  
Keyword(s):  
Biomass Burning ◽  
Atmospheric Chemistry ◽  
Forest Fires ◽  
El Niño ◽  
Tropospheric Ozone ◽  
Large Scale ◽  
El Nino ◽  
Global Burden ◽  
The North ◽  
Tropospheric O3

Abstract. We have studied the effects of the 2006 El Niño on tropospheric O3 and CO at tropical and sub-tropical latitudes measured from the OMI and MLS instruments on the Aura satellite. The 2006 El Niño-induced drought caused forest fires (largely set to clear land) to burn out of control during October and November in the Indonesian region. The effects of these fires are clearly seen in the enhancement of CO concentration measured from the MLS instrument. We have used a global model of atmospheric chemistry and transport (GMI CTM) to quantify the relative importance of biomass burning and large scale transport in producing observed changes in tropospheric O3 and CO. The model results show that during October and November biomass burning and meteorological changes contributed almost equally to the observed increase in tropospheric O3 in the Indonesian region. The biomass component was 4–6 DU but it was limited to the Indonesian region where the fires were most intense. The dynamical component was 4–8 DU but it covered a much larger area in the Indian Ocean extending from South East Asia in the north to western Australia in the south. By December 2006, the effect of biomass burning was reduced to zero and the observed changes in tropospheric O3 were mostly due to dynamical effects. The model results show an increase of 2–3% in the global burden of tropospheric ozone. In comparison, the global burden of CO increased by 8–12%.

Salvage logging in the boreal and cordilleran forests of Canada: Integrating industrial and ecological concerns in management plans

2009 ◽  
Vol 85 (1) ◽  
pp. 120-134 ◽  
Author(s):  
Michel Saint-Germain ◽  
David F Greene
Keyword(s):  
Forest Fires ◽  
Wood Decay ◽  
Significant Loss ◽  
Ecological Impacts ◽  
Decay Fungi ◽  
Wood Supply ◽  
Salvage Logging ◽  
The North ◽  
Starting Point ◽  
The Impact

Fire has been part of the North American boreal and cordilleran ecosystems for thousands of years. Because fire and harvesting compete directly for the same wood supply, and provinces have, within the last few decades, tended to reach their annual allowable cut, salvage logging has emerged as a practice to minimize the impact of fire on long-term wood supply. In most parts of the boreal and cordilleran forests, fire-killed boles rapidly degrade after their death, as wood-boring insects, stain, wood-decay fungi and checking lead to significant loss of grade or volume in the months following the fire. Because of this impending degradation, salvage operations are often hurried and other considerations, including the potential ecological impacts of salvage logging, have seldom been taken into consideration when defining harvesting strategies. The ecological consequences of rapid salvage have been widely studied only in the last 5 years, and it is now clear that salvage logging can have negative impacts on natural regeneration by seed, water quality, and fire-associated animal species. In this paper, we review both industrial and ecological constraints to salvage logging and discuss how both can be integrated in salvage plans. In particular, we focus on the issues of salvage timing and retention. At this point, some type of retention of merchantable stands, even if only for a few years, appears to be the only way to alleviate the negative ecological impacts of post-fire logging. On-site operational constraints, e.g., stands that cannot be harvested due to lack of accessibility, represent an important starting point for any retention strategy. Key words: boreal forest, forest fires, salvage logging, biodiversity, natural disturbances, regeneration after fire

scholarly journals Estimation of emissions from biomass burning in China (2003–2017) based on MODIS fire radiative energy data

2018 ◽  
Author(s):  
Lifei Yin ◽  
Pin Du ◽  
Mingxu Liu ◽  
Tingting Xu ◽  
Yu Song
Keyword(s):  
Biomass Burning ◽  
Forest Fires ◽  
Crop Residue ◽  
Crop Yields ◽  
Farming System ◽  
Radiative Energy ◽  
Vegetation Coverage ◽  
Fire Emissions ◽  
The North ◽  
Significant Downward Trend

Abstract. Biomass burning plays a significant role in air pollution and climate change. In this study, we used the method based on fire radiative energy (FRE) to develop a biomass burning emission inventory for China from 2003 to 2017. Daily fire radiative power (FRP) data in 1 km MODIS Thermal Anomalies/Fire products (MOD14/MYD14) were used to calculate FRE and combusted biomass. Available emission factors were assigned to four land-cover types: forest, cropland, grassland and shrubland. The farming system and crop types in different climate zones were taken into account in this research. Compared with traditional methods, the FRE method was found to provide a more reasonable estimates of emissions from small fires. The estimated average annual emission ranges, with a 90 % confidence interval, were 94.2 (78.7–117.6) Tg CO2 yr−1, 4.9 (2.5–8.3) Tg CO yr−1, 0.19 (0.05–0.51) Tg CH4 yr−1, 0.52 (0.18–0.81) Tg NMHC yr−1, 0.18 (0.04–0.39) Tg NOx yr−1, 0.07 (0.02–0.17) Tg NH3 yr−1, 0.03 (0.01–0.06) Tg SO2 yr−1, 0.04 (0.01–0.08) Tg BC yr−1, 0.3 (0.08–0.53) Tg OC yr−1, 0.49 (0.20–0.88) Tg PM2.5 yr−1, 0.56 (0.16–1.11) Tg PM10 yr−1. Forest fire was identified as the major source of the biomass burning emissions, and crop residue burning was the second highest contributor. In the 15-year study period, emissions from forest fires showed a significant downward trend. Crop residue emissions continued to rise until 2014, and then began to decline. Emissions from grassland and shrubland were little changed. Forest, grassland, and shrubland fires are mostly located in regions with high vegetation coverage, where the occurrence of fires is concentrated in arid seasons (spring and autumn). Plain areas with high crop yields, such as the North China Plain, experienced high agricultural fire emissions in harvest seasons. The resolution (daily, 1 km) of our inventory is much higher than previous inventories, such as GFED4s and GFASv1.0. It could be used in global and regional air quality modeling.

Sign in / Sign up

Export Citation Format

Share Document