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Progress in Physical Geography
Journal Prestige (SJR): 1.373
Citation Impact (citeScore): 4
Number of Followers: 13  
 
  Hybrid Journal Hybrid journal (It can contain Open Access articles)
ISSN (Print) 0309-1333 - ISSN (Online) 1477-0296
Published by Sage Publications Homepage  [1176 journals]
  • Soil erosion on arable land: An unresolved global environmental threat

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      Authors: John N Quinton, Peter Fiener
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Rationale and scope: Although soil erosion was recognised as a serious problem in antiquity and research into erosion started in the early 20th century, it remains a substantial problem for agriculture and the environment across the globe. It disrupts agricultural production, threatening food production, increases the severity of floods and droughts and impacts on soil biology and biogeochemical cycling. This review describes the different processes and manifestations of erosion on arable land and the availability of global data. It points out that while there is a good understanding of the processes of erosion, the causes are complex and even if agronomic and landscape solutions are available, their implementation is challenging and needs tailored approaches to account for the specific local socio-economic, political, and institutional contexts.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-11-24T04:39:13Z
      DOI: 10.1177/03091333231216595
       
  • Observing coastal wetland transitions using national land cover products

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      Authors: Nicholas M Enwright, Michael J Osland, Karen M Thorne, Glenn R Guntenspergen, James B Grace, Greg D Steyer, Nate Herold, Bogdan Chivoiu, Minoo Han
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Over the coming century, climate change and sea-level rise are predicted to cause widespread change to coastal wetlands. Estuarine vegetated wetlands can adapt to sea-level rise through both vertical development (i.e., biophysical feedbacks and sedimentation) and upslope/horizontal migration. Quantifying changes to estuarine vegetated wetlands over time can help to inform current and future decisions regarding land management and resource stewardship. In this study, we show how coastal land cover maps readily available in the US can be used to assess and understand estuarine vegetated wetland changes. This assessment involves two steps: (1) identifying the net gain/loss of estuarine vegetated wetlands and (2) determining which land cover types contribute to the net gain/loss. From this information, we developed estuarine vegetated wetland change scenarios that evaluate whether estuarine vegetated wetland gain kept up with loss and whether the contribution was from: (1) estuarine vegetated wetland migration or tidal restoration; (2) land building (i.e., development); or (3) both. We assessed changes from 1996 to 2016 for: (1) the conterminous US; (2) each major US coastline; and (3) focal estuaries with the most change per coast. We found that the change scenario (1, 2, or 3) varied across coastlines. Moving forward, national coastal land cover programs can be informed by utilizing methodologies that leverage contemporary information for delineating the estuarine zone from upslope/adjacent wetlands. We highlight approaches that could be used to address this challenge and provide complementary information related to wetland condition changes.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-11-20T10:35:03Z
      DOI: 10.1177/03091333231216588
       
  • Considering the dynamics of water surface boundaries to measure the
           evolution of hydrological connectivity in the Yangtze River Delta, China

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      Authors: Zhenya Li, Fanhua Kong, Haiwei Yin, Michael E Meadows, Xiaojun Yang, Kejing Zhou, Jie Su
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Dynamics of the terrestrial water surface impact hydrological connectivity. Compared with traditionally deployed water surface parameters, changes in the water-boundary more effectively account for the dynamics of water surface and depth resulting from hydrological variations. However, previous studies of hydrological connectivity generally applied only connectivity length or width parameters using the center line of the water body and therefore fail to fully capture the impact of water boundary dynamics. In this study, optimized water body extraction indices based on data obtained from remote sensing imagery are used to develop a novel metric that indicates water surface boundary dynamics and reveal surface hydrological connectivity changes in the Yangtze River Delta from 1990 to 2020. Detailed inter-annual and seasonal changes in the evolution of water body boundaries from a water surface perspective indicate an overall decline in hydrological connectivity against the background of climate change, increased urbanization, and dam construction. The declining trend in connectivity occurs in three phases, viz. from 1990 to 2003, a gradual decline is exhibited but with a very marked degree of inter-seasonal variability; between 2003 and 2012, connectivity remains relatively constant but with a reduced amplitude between seasons; further reductions in the magnitude of seasonal variations characterize the third phase, to 2020. Meanwhile, the stability of hydrological connectivity, indicated by the coefficient of variation, also exhibits marked spatial heterogeneity. Parts of the delta with more tributaries, including the Huaihe and southeastern basins, have lower stability (7.33 and 6.59, respectively) than the Yangtze basin (6.22). This study presents a novel metric to achieve greater precision in the monitoring of hydrological connectivity. Such information can be harnessed to improve regional ecological and water resource management.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-11-15T11:32:32Z
      DOI: 10.1177/03091333231213536
       
  • Large floods on the lower Ohio River inferred from slackwater deposits

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      Authors: Charlotte Wiman, Tessa Harden, Zhixiong Shen, B. Brandon Curry, Joeri B Reinders, R. Edward Beighley, Samuel E Muñoz
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Slackwater deposits representing past flood events provide a robust means to extend systematic gage records further back in time, place historic floods in a longer-term context, and reduce uncertainties in flood hazard analysis. The identification and application of slackwater deposits in riverine paleoflood hydrology has traditionally been limited to arid bedrock-controlled environments and periglacial environments. In this study, we utilize methods developed in humid alluvial settings and apply them to slackwater deposits, one of the first studies to do so. This novel approach uses sediment texture and geochemistry to distinguish slackwater deposits from in situ material in a temperate alluvial setting. We identify multiple slackwater deposits in two rock shelters situated on bluffs adjacent to the lower Ohio River. Flood age estimates are based on optically stimulated luminescence (OSL) dating, and discharge estimates are based on a 1D HEC-RAS model. The uppermost slackwater deposit at both sites corresponds to the AD 1937 historic flood of record (∼31,400 m3/s), while another slackwater deposit identified only at the lower elevation site corresponds to a paleoflood that occurred around AD 1650 with a discharge of ∼23,900 m3/s. Our findings imply that the AD 1937 flood represents the largest magnitude flood on the lower Ohio River in at least the last 400 years. Inclusion of the paleoflood into a flood frequency analysis for the Ohio River at Louisville reduces uncertainties in large flood quantiles by ∼50%.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-10-26T06:16:01Z
      DOI: 10.1177/03091333231208612
       
  • Soil stabilization by integrating dust particles with calcium
           lignosulphanate

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      Authors: Velagapalli Chiranjeevi, Kamal Singh, D Kishan
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      This paper analyzes the stabilizing effect of stone dust, granite dust, marble dust, and calcium lignosulphonate on construction materials and natural soils during road construction. The ultimate aim was to enhance the soil’s engineering properties such that the pavement constructed could correctly withstand the load applied. To achieve this, every stabilizer was amalgamated with the soil at various percentages between 5 and 50%. Measurements were made of Atterberg limit tests, moisture content, and specific gravity. The research demonstrated that a diminution in optimal moisture content was seen, with an elevation in maximum dry density and California bearing ratio (CBR). Enhancements in the unconfined compressive strength were also identified. The outcomes determined that the untreated soil’s CBR was 2.27% and in the case of soil with 45% additives, the CBR attained was 5.05%. When the soil was mixed with 50% additives, performance of 30.21%, 17.42%, and 12.82% was exhibited for (a) liquid limit, (b) plastic limit, and (c) plasticity index. Moreover, via the addition of presented stabilizers, the soil’s mechanical properties were elevated appreciably.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-10-23T02:14:06Z
      DOI: 10.1177/03091333231209157
       
  • A landscape-level study on vegetation richness of ancient landslide areas

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      Authors: Sadao Takaoka
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Landslides have received significant attention as an important natural disturbance that maintains biodiversity, but most previous studies have focused on the early stages of succession during years or decades in sites or small watersheds. The present study aimed to determine what regional drivers influence long-term ecological succession in large, ancient landslide scarps across a mountainous region in Japan. A landscape-level analysis of 993 landslide scarps using GIS revealed that climatic factors, especially snowfall, are important regional drivers of vegetation development on landslide head scarps in the region. While vegetation has developed on ancient landslide scarps, not all of them have returned to their pre-landslide vegetation state even though hundreds or thousands of years may have passed. The relationship between the number of vegetation types and maximum snow depth shows that where the maximum snow depth is less than 100 cm, more than 50% of the landslide scarps are covered by one type of vegetation, and the percentage of scarps covered by one type of vegetation decreases with increasing snow cover. The deeper the snow, the more vegetation types tend to develop on the landslide scarps. Since forest vegetation cannot develop due to heavy snow, meadows, grasslands, and shrublands are found on the scarps. It is concluded that the combined effects of both landslide-caused disturbances and climatic factors are creating regional diversity in vegetation types.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-10-14T12:00:53Z
      DOI: 10.1177/03091333231206314
       
  • Comprehensive evaluation of urban development suitability based on
           constraints and development factors: A case study of the central urban
           area of Zhengzhou, China

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      Authors: Zhenqin Shi, Jingeng Huo, Wenbo Zhu, Ran Ma, Hua Xue, Zechen Wang
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      The overcapacity and overdevelopment of cities have led to various environmental hazards and resource depletion, making it crucial to evaluate the suitability of urban development. This research field provides scientific evidence and policy recommendations to improve land use quality and distribution. However, contemporary studies solely focus on construction land versus non-construction land competition, ignoring potential constraints from agriculture and ecology on parcel development. Using the land use situation of Zhengzhou City, this study comprehensively evaluated urban development suitability through hierarchical analysis, Delphi method, and eight-direction analysis. A multi-attribute overlay was applied with spatial restrictions from ecological protection and agricultural production, combined with urban expansion and development conditions. The results indicated that: (1) Ecological protection was critical for sustainable urban development, and areas like the Yellow River coast, northwest wetland, and southwest woodland were significant for ecological protection. High suitability areas for agricultural production were primarily located within the existing cultivated land. (2) Regarding urban expansion, the southeast of the city center was identified as the most suitable area, mainly covered by dryland. (3) Overall, the unsuitable, basically unsuitable, medium, suitable, and highly suitable areas for urban development covered 244, 921, 3024, 2224, and 944 km2, respectively. (4) The southeast-northwest direction showed prominent spatial characteristics for urban development suitability, while intensive development mode dominated the east-west direction of the city center. These findings provide significant guidance for land development and utilization, optimizing the spatial pattern, and formulating policies in Zhengzhou. Nevertheless, the weight calculation process presents a subjective factor that needs to be addressed in future research. More objective weight calculation results are necessary to achieve a more scientifically rigorous evaluation of urban development suitability.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-10-03T12:13:22Z
      DOI: 10.1177/03091333231180805
       
  • Human impacts on vegetation carbon sequestration capacity in the Qilian
           Mountains, northeastern Tibetan Plateau since 2000

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      Authors: Biao Zeng, Fuguang Zhang, Ying Cao, Yanqi Shen, Zhenhua Meng
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Vegetation carbon sequestration in alpine areas of West China, such as the Qilian Mountains on the northeastern Tibetan Plateau, has been subject to long-term human intervention under a warming climate since the launch of the western development strategy (WDS) in 2000. However, the human impacts on vegetation carbon sequestration capacity during this period remain unclear. In this study, the magnitude and direction of human impacts on vegetation carbon sequestration capacity (defined as net primary production, NPP) were assessed by the deviation of remote-sensing–estimated actual NPP data from the simulated potential NPP. The potential value was derived from natural system coupling under the assumption that human activities ceased during the assessment period. The impacts of natural forces and historic human activities were then effectively exfoliated in our final assessment using a process-based IBISi model. The results indicate that the total actual vegetation carbon sequestration capacity in the Qilian Mountains has reduced compared with its potential value since the WDS launched. This reduction was mainly attributed to grazing in the grasslands. However, deforestation, mineral resource exploitation, and the construction of hydropower facilities have also caused a reduction in vegetation carbon sequestration capacity at the local scales. In contrast, forestry protections and afforestation, and agricultural activities associated with reclamation, cultivation, irrigation, and fertilization, have resulted in local increases in the vegetation carbon sequestration capacity in the corresponding forest lands, shrublands, and croplands. These findings highlight the importance of ecological protections for vegetation carbon sequestration and were expected to provide evidence to verify the improvement of ecological management and the increasing of carbon sinks in West China.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-09-06T06:38:54Z
      DOI: 10.1177/03091333231201025
       
  • Prehistoric human occupation and adaptation on the hinterland of the
           Tibetan Plateau in the Early Holocene

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      Authors: Sunmei Jin, Guangliang Hou, Youcheng Chen, Hong Qiao, Bin Han, Chongyi E, Zhuoma LanCuo, Jingyi Gao, Zhuoma WenDe
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      The occupation process and survival strategies of prehistoric humans on the Tibetan Plateau are important scientific questions for understanding human adaptation to extreme high-altitude environments. Here, we report a newly discovered microlithic site at Daiqu (DQ) in the Tongtian River basin of the central-eastern plateau. We collected 239 lithic artifacts from the DQ site for typological analysis. OSL and AMS14C dating samples were collected from the human active layer. Lipid residues from hearth sediments were analyzed, and we simulated and assessed environmental extremity and route accessibility for the site. Dating results suggest that the stable sedimentary layers began to form around 10.96 ± 0.56 ka BP at the DQ site. Human activity at DQ as early as 9271 ± 143 cal a BP, making it the earliest reported Holocene site with accurate stratigraphic dating on the plateau hinterland to date. Hearths and lithic artifacts indicate that the DQ site was a frequently used seasonal hunting camp, where quality lithic raw material was obtained and microliths processed. Prehistoric humans occupying the site relied on non-ruminant terrestrial animals as food resources. The DQ site is ideally situated to serve as a transit station for hunter-gatherers as they migrated between high and low elevations. Ameliorating Holocene climate promoted prehistoric human exploration of more environmentally extreme areas.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-08-25T03:33:41Z
      DOI: 10.1177/03091333231197168
       
  • Ensemble learning based on remote sensing data for monitoring agricultural
           drought in major winter wheat-producing areas of China

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      Authors: Lunche Wang, Yuefan Zhang, Xinxin Chen, Yuting Liu, Shaoqiang Wang, Lizhe Wang
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Drought is mainly triggered by the lack of precipitation, which can lead to insufficient water supply for crops thus affecting their growth and development. Reliable drought monitoring is crucial to understanding drought risk and avoiding drought-induced crop yield losses. Based on the Stacking regression method and multiple remotely-sensed drought factors from 2001 to 2017, this study developed an ensemble learning framework for monitoring agricultural drought in major winter wheat-producing areas in China. Stacking used five machine learning algorithms, namely, extreme gradient boosting, support vector regression, extra trees, and multi-layer perceptron, as the base learners to model the relationship between remote sensing drought factors and 1-, 3-, and 6-month standardized precipitation evapotranspiration index (SPEI). In this study, county-level winter wheat yield records and drought maps provided by the Global SPEI database (SPEIbase) were adopted to assess the suitability of Stacking-predicted SPEI drought maps in agricultural drought monitoring. The results show that Stacking outperformed other machine learning algorithms in terms of estimation accuracy, with the highest R2 value of 0.77 and the lowest root mean square error (RMSE) of 0.47. The longer the time scale of model-predicted SPEI, the higher its correlation with detrended winter wheat yields. The comparison with the drought maps of SPEIbase shows that the Stacking-predicted drought maps successfully captured the spatial pattern and intensity change of drought events. The approach presented in the study has good applicability for agricultural drought monitoring and could be extended to the rest of the areas.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-08-16T05:32:00Z
      DOI: 10.1177/03091333231188814
       
  • Environmental heterogeneity as a driver of terrestrial biodiversity on a
           global scale

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      Authors: Ji-Zhong Wan, Chun-Jing Wang, Pablo A Marquet
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      To improve the effectiveness of biodiversity conservation and risk assessments under global changes, it is necessary to understand the drivers of terrestrial biodiversity on a global scale. Environmental heterogeneity is an important umbrella term for different environmental factors that contribute to species diversity. Previous studies have shown that there are significant relationships between geodiversity and biodiversity on a global scale, and that heterogeneity in geodiversity features and environmental variables, that is indicators of environmental heterogeneity (EH), drive biodiversity at local and regional scales. However, we do not yet know how terrestrial biodiversity is maintained, how well represented are the different taxa, and where would they be more at risks considering their abundances and diversities. In this study, we quantified EH of climate, topography, and land cover. We used four theoretical indexes (i.e., Fisher’s alpha, Shannon’s H, Hurlbert’s PIE, and Good’s u) to quantify terrestrial biodiversity based on abundance and diversity. We used regression models to explore the relationships between environmental heterogeneity and terrestrial biodiversity across different organismic groups (ants, bats, birds, butterflies, frogs, ground beetles, mosquitoes, odonates, orthopterans, rodents, scarab beetles, and trees) globally. We found significant relationships between environmental heterogeneity and terrestrial biodiversity, particularly for trees across the three EH components (climate, topography, and land cover), however, the effects of environmental heterogeneity on terrestrial biodiversity may vary among different groups of organisms. Land cover EH could affect the terrestrial biodiversity for ants, bats, birds, butterflies, frogs, mosquitoes, odonates, orthopterans, rodents, and scarab beetles. Furthermore, there were significant relationships between topographic EH and the terrestrial biodiversity for bats, butterflies, ground beetles, odonates, and trees. Climatic EH had significant effects on the terrestrial biodiversity for all organism groups. Our study provides new insights into biodiversity conservation by considering the terrestrial biodiversity based on EH, an indicator of geodiversity.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-08-11T02:37:21Z
      DOI: 10.1177/03091333231189045
       
  • Go or grow' Feedbacks between moving slopes and shifting plants in
           high mountain environments

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      Authors: Jana Eichel, Markus Stoffel, Sonja Wipf
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      High mountains are climate change hotspots. Quickly rising temperatures trigger vegetation shifts such as upslope migration, possibly threatening mountain biodiversity. At the same time, mountain slopes are becoming increasingly unstable due to degrading permafrost and changing rain and snowfall regimes, which favour slope movements such as rockfall and debris flows. Slope movements can limit plant colonization, while, at the same time, plant colonization can stabilize moving slopes. Thus, we here propose that response of high mountain environments to climate change depends on a ‘biogeomorphic balance’ between slope movement intensity and the trait-dependent ability of mountain plants to survive and stabilize slopes. We envision three possible scenarios of biogeomorphic balance: (1) Intensifying slope movements limit vegetation shifts and thus amplify instability. (2) Shifting ecosystem engineer species reduce slope movement and facilitate shifts for less movement-adapted species. (3) Trees and tall shrubs shifting on stable slopes limit slope instability but decrease biodiversity. Previous geomorphic, ecological and palaeoecological studies support all three scenarios. Given differences in ecologic and geomorphic response rates to climate change, as well as high environmental heterogeneity and elevational gradients in mountain environments, we posit that future biogeomorphic balances will be variable and heterogeneous in time and space. To further unravel future biogeomorphic balances, we propose three new research directions for joint research of mountain geomorphologists and ecologists, using advancing field measurement, remote sensing and modelling techniques. Recognizing high mountains as ‘biogeomorphic ecosystems’ will help to better safeguard mountain infrastructure, lives and livelihoods of millions of people around the world.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-08-09T01:09:34Z
      DOI: 10.1177/03091333231193844
       
  • Identification of priority areas for soil erosion control based on minimum
           administrative units and karst landforms in karst areas of Guizhou

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      Authors: Jun Jing, Rui Li, Yushan Zhang, Qinglin Wu
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Soil erosion is one of the most serious ecological threats in karst areas of Southwest China. The identification of priority areas for remediation and its driving factors is essential to improving the efficiency of prevention and control. The present study systematically considered natural and socio-economic factors not involved in the revised universal soil loss equation (RUSLE) model, and determined priority areas for soil erosion management based on minimum administrative units and karst landforms. Then, the driving factors were identified by using geographic detector. The results showed that the priority areas were mainly concentrated in the southwest, southeast and northeast, overlapping with the severely eroded areas (Erosion rate=45.79 t·ha−1·a−1). Gradient risk zones had geomorphological differences, but the most eroded zones were all controlled by bedrock exposure rates, elevation, or slope position. The spatial correlation and high erosion rate of priority areas provided opportunities to optimize the efficiency and cost of control. Driving factors were affected by karst landforms. The explanation power of slope position on soil erosion was higher in the peak cluster depressions and karst basins with small undulations ([math]), while the karst gorges, trough valleys and plateaus with large undulations gradually decreased ([math]). The interaction of driving factors will enhance the explanatory power for soil erosion. Among them, the repetition rate of elevation was 60%, and the repetition rate of lithology and development index was 40%. This study provides useful information for identifying and managing priority areas for soil erosion control, and enriches the theory of soil and water conservation in karst areas.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-07-15T01:51:03Z
      DOI: 10.1177/03091333231189350
       
  • The evolution of open biomass burning during summer crop harvest in the
           North China Plain

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      Authors: Shiyu Li, Ming Zhang, Lunche Wang, Qian Cao, Wenmin Qin
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Open biomass burning (OBB) negatively impacts air quality by discharging abundant fine particulate matter (PM2.5, aerodynamic diameter ≤2.5 µm) and trace gases. The statistical methods and numerical simulations have been used to estimate emissions from OBB. The former is poor in producing reliable distributions and transport of emissions, while studies with the latter have focused on cases analysis over short periods. This study investigates the multi-year evaluation of OBB and its contribution to PM2.5 and black carbon (BC) based on satellite observations and numerical modeling over the North China Plain. The number of fires increased by 206% from 2008 to 2012, and decreased by 84% from 2012 to 2016, indicating that the implementation of straw burning ban policy had achieved significant positive effects. The simulation from Weather Research and Forecasting model coupled with chemistry showed that the surface concentrations of PM2.5 and BC emitted by OBB in the burning source area increased from 22 and 3.22 μg/m3, respectively, in 2008 to 45.77 and 6.47 μg/m3, respectively, in 2012, and then decreased to 1.41 and 0.22 μg/m3, respectively, in 2016. The differentiated impacts on air quality of policies across provinces are also investigated. Open crop straw burning was banned early in Shandong and Henan provinces, but they suffer from poor air quality due to open straw burning until the effective straw burning ban in Anhui and Jiangsu provinces, which suggests the need for interregional collaboration for pollution control.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-07-13T10:33:39Z
      DOI: 10.1177/03091333231187817
       
  • The roles of environmental conditions in the pollutant emission-induced
           gross primary production change: Co-contribution of meteorological fields
           and regulation of its background gradients

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      Authors: Xuan Gui, Lunche Wang, Qian Cao, Shiyu Li, Weixia Jiang, Shaoqiang Wang
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Anthropogenic emissions affect vegetation photosynthesis and carbon flux through meteorological variations induced by aerosols and clouds. However, the insufficient consideration of meteorological conditions limits the understanding of relevant mechanisms, and further inhibits the projection of future terrestrial carbon balance. Based on multiple sets of model simulations, we characterized changes in gross primary production (GPP) due to three typical individual pollutants emissions (black carbon, organic carbon, and sulfate), quantified the relative contributions of co-varied environmental factors, and explored the regulatory roles of background meteorological conditions across China. Our results showed that the heterogeneous GPP enhancement induced by emissions was dominated by cloud cover (CC) change. During its short-term effect, air temperature (Tair), vapor pressure deficit (VPD), and radiation (both quality and quantity) played a collectively non-negligible role in GPP variation, among which the universal diffuse radiation fertilization effect was generally far less than the benefits of brighter, cooler, and wetter environmental conditions. However, the sensitivity of GPP to an individual environmental variable was also altered by background meteorological gradients, whose changing pattern differed substantially among factors, indicating that the meteorological-regulated vegetation optimal photosynthetic range was a trade-off among heat, water, and light instead of being controlled by the univariable. This study implies that a deeper understanding of concurrent environmental variables is an effective way to reduce uncertainties in assessing the terrestrial carbon cycle perturbation exerted by human-induced emissions, especially under future scenarios with ongoing climate change.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-07-11T04:24:57Z
      DOI: 10.1177/03091333231186893
       
  • Experimental and numerical investigation on the hydraulic design criteria
           for a step-pool nature-like fishway

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      Authors: Sruthi T Kalathil, Venu Chandra
      Abstract: Progress in Physical Geography: Earth and Environment, Ahead of Print.
      Hydraulic considerations specific for the design of step-pool nature-like fishways (NLFs) are limited to the body dimensions of the target species. Additional hydraulic criteria for flow depth, maximum values for each of pool depth, velocity, and turbulent kinetic energy in terms of the weir opening width and discharge can help design an optimum step-pool NLF. The present study developed design charts and rating curves based on numerical modeling using the computational fluid dynamics software FLOW-3D® HYDRO. Instantaneous velocity measurements on a 1:4 scaled physical model of a step-pool nature-like fishway designed as per the available design guidelines have been used to validate the numerical model. The hydrodynamics of the fishway with respect to the weir opening ratio br (0.10, 0.25, 0.45, 0.65, and 1.00) and discharge Q (0.1–1.5 m3/s) was analyzed through numerical simulations on a prototype scale. The simulation results showed that the maximum flow velocity and the averaged velocity over the crest at br = 0.10 and 0.25 are considerably lower than at br> 0.25. The maximum turbulent kinetic energy and energy dissipation factors for the tested range of discharges were within recommended limits for br = 0.10 and 0.25. The present study outcome in terms of the design charts and rating curves that illustrate the relationship between different variables can be used for an optimum design and ease in field implementation. In addition, the bed structure of the step-pool NLF presented in this study can be used to recreate full-scale or pilot models.
      Citation: Progress in Physical Geography: Earth and Environment
      PubDate: 2023-07-07T07:49:41Z
      DOI: 10.1177/03091333231187619
       
 
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