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A case study of exceptionally heavy rainfall event over Uttarakhand, India on 18th October, 2021 and its forecasting 2021年10月18日印度北阿坎德邦异常强降雨事件及其预测案例研究
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.4754
R. Thapliyal, Bikram Singh
The unprecedented rainfall observed over Uttarakhand on 18th October 2021 caused landslides, debris flow and floods over the Kumaun region and adjoining districts of the Garhwal region of Uttarakhand, which resulted in huge damage to life, agriculture, transport, tourism and other sectors. The synoptic and dynamic study of the current event showed the movement of the Low-Pressure Area over central India resulting in the strong southeasterly winds (Atmospheric River) over Indo-Gangetic planes from the Bay of Bengal from 17th to 19th October. The interaction and blocking of the Atmospheric River by the deep trough of eastward-moving Western Disturbance (WD) caused extreme rainfall over Uttarakhand. However, the X-band Doppler Weather Radar and 123 Automatic Weather/raingauge Stations data suggest that the hourly rainfall rate was of light to moderate intensity (10-20 mm/h) over most of the area and at most of the time. The rainfall rate was extremely intense (50-100 m/hour) for around 1-hour duration in 7 stations of Udham Singh Nagar, Champawat, Nainital and Pauri districts. Unlike the June 2013 extremely heavy rainfall event over Uttarakhand which impacted the whole Uttarakhand state, the present event was concentrated over the Kumaun region and the highest ever 24-hours accumulated rainfall was observed on 18th October, 2021 in Kumaon region of Uttarakhand. The expected rainfall as well as the impact of the event over Uttarakhand was forecasted 5 days in advance with good accuracy based on the synoptic analysis and NWP model guidance. The predictability of the IMD-GFS (T-1534) NWP model was found to be up to 10 days for this extreme rainfall event.
2021年10月18日,在北阿坎德邦观测到前所未有的降雨,导致库曼地区和北阿坎德邦加尔瓦尔地区邻近地区发生山体滑坡、泥石流和洪水,对生命、农业、交通、旅游和其他部门造成巨大破坏。本次事件的天气学和动力学研究表明,10月17日至19日,印度中部低压区的运动导致孟加拉湾的印度-恒河平面上出现强烈的东南风(大气河)。东移的西部扰动(WD)深槽对大气河的相互作用和阻塞造成了北阿坎德邦的极端降雨。然而,x波段多普勒天气雷达和123个自动天气/雨量站资料显示,在大部分地区和大部分时间,每小时降雨量为轻至中等强度(10-20毫米/小时)。在Udham Singh Nagar、champaat、Nainital和Pauri地区的7个站点,持续约1小时的降雨量非常强(50-100米/小时)。与2013年6月北阿坎德邦发生的影响整个北阿坎德邦的特大降雨事件不同,这次事件集中在库曼地区,2021年10月18日在北阿坎德邦的库曼地区观测到有史以来最高的24小时累积降雨量。在天气分析和NWP模式指导下,提前5天预报了北阿坎德邦的预期降雨量和事件的影响,预报精度较高。发现IMD-GFS (T-1534) NWP模式对这次极端降雨事件的可预测性高达10天。
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引用次数: 0
Studies on the variation in concentrations of respirable suspended particulate matter (PM10), NO2 and SO2 in and around Nagpur 那格浦尔及其周边地区可吸入悬浮颗粒物(PM10)、NO2和SO2浓度变化的研究
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.828
Divyansh Saini, D. Lataye, V. Motghare
The objective of this study is to assess the long-term variation in concentrations of Respirable suspended particulate matter (PM10), sulphur dioxide (SO2) and nitrogen dioxide (NO2) in the ambient air of Nagpur (India) during 2011-2018. The pollution data during the above period at three locations, viz., residential (Station-I), industrial (Station-II), and commercial location (Station-III) has been analyzed. The highest daily average concentration of PM10 at residential, industrial, and commercial locations was found 154 microgm/m3, 199 microgm/m3, and 153 microgm/m3, whereas, the average annual concentration at these locations was found 101.87 microgm/m3, 115.37 microgm/m3 and 98.75 microgm/m3, respectively during the above period. The highest daily average concentration of SO2 was found at 18 microgm/m3, 22 microgm/m3 and 19 microgm/m3 and the average annual concentration was 13.25 microgm/m3, 13.5 microgm/m3, 13 microgm/m3 at respective locations. And the highest daily average concentration of NO2 was found 77 microgm/m3, 60 microgm/m3, 60 microgm/m3 and the annual average concentration was 44.125 microgm/m3, 41.825 microgm/m3 and 40.25 microgm/m3 at the respective locations. The exceedance factors for PM10 varied from 'moderate to high' at the residential and commercial locations and from 'high to moderate' at the industrial location. Planetary boundary layer height (PBLH) and ventilation coefficient (VC) were also estimated over the region for 2011-2018. The maximum PBLH and VC observed during the study period was in the summer season, and the minimum was in the post-monsoon season. Annual and Seasonal Air quality index analysis shows that the level of pollution was in the range of SATIFACTORY to MODERATE. A study of seasonal analysis of PM10, SO2 and NO2 showed that the higher concentrations were found in winter relative to summer with the least concentration occurring during the monsoon season. A regression analysis was performed to check PM10's interdependence with other contaminants. A positive association was found between PM10 and SO2 for all seasons. A negative association was found between PM10 and NO2 in summer for all the stations and winter at Station-I and Station-III. Similarly, the correlation between PM10 and meteorological parameters such as wind speed and temperature was found to be negative whereas it was positive for relative humidity.
本研究的目的是评估2011-2018年印度那格浦尔环境空气中可吸入悬浮颗粒物(PM10)、二氧化硫(SO2)和二氧化氮(NO2)浓度的长期变化。分析了上述期间住宅(监测站一)、工业(监测站二)和商业(监测站三)三个地点的污染数据。住宅、工业和商业场所PM10日平均浓度最高,分别为154、199和153微克/立方米,年平均浓度最高,分别为101.87、115.37和98.75微克/立方米。SO2的日平均浓度最高为18、22和19微克/m3,年平均浓度分别为13.25、13.5和13微克/m3。NO2日平均最高浓度分别为77、60、60微克/m3,年平均浓度分别为44.125、41.825、40.25微克/m3。住宅和商业地点的PM10超标系数从“中等到高”,工业地点的超标系数从“高到中等”。估算了该区域2011-2018年的行星边界层高度(PBLH)和通风系数(VC)。研究期间观测到的PBLH和VC在夏季最大,在季风后季节最小。年度和季节性空气质量指数分析表明,污染水平在满意到中等范围内。PM10、SO2和NO2的季节分析表明,冬季浓度高于夏季,季风季节浓度最低。进行回归分析以检查PM10与其他污染物的相互依赖性。PM10和SO2在所有季节都呈正相关。夏季各站点PM10与NO2呈负相关,冬季1、3站点PM10与NO2呈负相关。同样,PM10与风速、温度等气象参数呈负相关,而与相对湿度呈正相关。
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引用次数: 0
A Geographic Information System (GIS) based approach for drainage and morphometric characterization of Beki river basin, India 基于地理信息系统(GIS)的印度贝基河流域排水和形态特征分析方法
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.5608
M. Mazumdar, M. Dutta, Mrigakshi Bharadwaj
Geographic Information Systems and remote sensing, have proved to be efficient tools in delineation of drainage pattern and different geometric methodology of geomorphologic, watershed management even GIS has been widely used in several flood management, and environmental applications. The river Beki with an area of 19,354.35 sq.km2 originates at Himalayan glacier (Kula Kangri glacier in Bhutan) 26.18° N latitudes and 90.53° E longitudes and flows though the plains of Assam and finally to the mighty Brahmaputra at 26.48° N latitudes and 91.02° E longitudes has been selected for detailed morphometric analysis. Morphometric parameters via; Stream order, Stream length, Bifurcation ratio, Drainage density, Drainage frequency, Drainage texture, Form factor, Circularity ratio, Elongation ratio and Compactness ratio etc. were measured for prioritization and compound parameter values were calculated. This study will help the local people to utilize the resources in right manner for Sustainable Water Resource Development of the Basin area. Moreover, the study can also be referred as a benchmark for studies on temporal change in geomorphology due to climate change. Different Morphometric analysis provides the explanation of physical characteristics of the watershed which are useful for the areas of land use planning, soil conservation, terrain elevation and soil erosion.
地理信息系统和遥感,已被证明是有效的工具,在描绘流域格局和不同的几何方法的地貌,流域管理,甚至GIS已被广泛应用于一些洪水管理和环境应用。贝基河面积19354.35平方公里。km²起源于喜马拉雅冰川(不丹的Kula kangi冰川),北纬26.18°,东经90.53°,流经阿萨姆邦平原,最终流入北纬26.48°,东经91.02°的雅鲁藏布江,进行详细的形态计量学分析。形态计量参数via;通过测量水流顺序、水流长度、分叉比、排水密度、排水频率、排水纹理、形状因子、圆度比、伸长率、密实比等进行优先级排序,并计算复合参数值。本研究将有助于当地居民合理利用资源,实现流域水资源的可持续发展。此外,该研究也可以作为气候变化引起的地貌时间变化研究的基准。不同形态计量学分析提供了对流域物理特征的解释,对土地利用规划、土壤保持、地形高程和土壤侵蚀等领域具有重要意义。
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引用次数: 0
Different statistical models based on weather parameters in Navsari district of Gujarat 基于古吉拉特邦Navsari地区天气参数的不同统计模型
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.3495
Y. Garde, K. Banakara, H. Pandya
Agriculture plays very important role in development of country. Rice is a staple food for more than half of world’s population. Timely and reliable forecasting provides vital and appropriate input, foresight and informed planning. The present investigation was carried out to forecast Kharif rice yield using two different statistical techniques, viz., discriminant function analysis and logistic regression analysis. The statistical models were developed using data from 1990 to 2012 and validation of developed models was done by using remaining data, i.e., 2013 to 2016. It was observed that value of adjusted R2 varied from 73.00 per cent to 93.30 per cent in different models. The best forecast model was selected based on high value of adjusted R2, Forecast error and RMSE. Based on obtained results in Navsari district, the discriminant function analysis technique (Model-5) was found better than logistic regression analysis (Model-12) for pre-harvest forecasting of rice crop yield. The results revealed that Model-5 showed comparatively low forecast error (%) along with highest value of Adj. R2 (93.30) and lowest value of RMSE (120.07). Also Model-5 is able to generate yield forecast a week earlier (39thSMW) than Model-12 (40thSMW). 
农业在国家的发展中起着非常重要的作用。大米是世界上一半以上人口的主食。及时和可靠的预测提供了重要和适当的投入,远见和明智的计划。本研究采用判别函数分析和logistic回归分析两种不同的统计技术对水稻产量进行预测。利用1990 - 2012年的数据建立统计模型,利用2013 - 2016年的剩余数据对建立的模型进行验证。据观察,在不同的模型中,调整后的R2的值从73.00%到93.30%不等。根据调整后的R2、预测误差和RMSE的高值选择最佳预测模型。基于Navsari地区的结果,判别函数分析技术(模型5)比logistic回归分析(模型12)更适合水稻作物收获前产量预测。结果表明,模型5预测误差较低(%),相对值R2最高(93.30),RMSE最低(120.07)。此外,模型-5能够比模型-12 (40 smw)提前一周(第39 smw)生成产量预测。
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引用次数: 0
Modeling medium resolution evapotranspiration using downscaling techniques in north-western part of India 用降尺度技术模拟印度西北部中分辨率蒸散发
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.5112
Arvind Dhaloiya, Darshana Duhan, D. Denis, Dharmendra Singh, Mukesh Kumar, Manender Singh
The present investigation provides a modeling solution to downscale MODIS-based evapotranspiration (ET) at a 30 m spatial resolution from its original 500 m spatial resolution using meteorological and Landsat 8 (Operational Land Imager, OLI) data by employing downscaling models. The nine indices namely Surface Albedo, Land Surface Temperature (LST), Normalized Difference Vegetation Index (NDVI), Soil-Adjusted Vegetation Index (SAVI), Modified Soil-Adjusted Vegetation Index (MSAVI), Normalized Difference Built-up Index (NDBI), Normalized Difference Water Index (NDWI), Normalized Difference Moisture Index (NDMI), and Normalized Difference Infrared Index for Band 7 (NDIIB7) were calculated from Lansat 8 data at 30 m spatial resolution. The multiple linear regression (MLR) and Least Square Support Vector Machine (LS-SVM) models were developed to generate the relationship between MODIS 500 m ET and Landsat indices at 500 m scale. Further, these develop models were used to estimate 30 m ET based on 30 m Landsat 8 indices. The performance of developed models (MLR and LS-SVM) was carried out using correlation coefficient (CC), Nash-Sutcliffe coefficient (NASH) efficiency, Root Mean Square Error (RMSE) and Normalised Mean Square Error (NMSE). Penman–Monteith (PM) method was used to estimate the ET using observed station data. The results show that lowest ETO was observed in the month of December while it was maximum in the month of May. Using the performances indices, it was found that LS-SVM model slightly outperformed than MLR model. However, the downscaled model overestimates ET in comparison to the Penman-Monteith method. Further, the significant correlation was found between MODIS ET and LS-SVM ET at all the stations.
本研究利用气象和Landsat 8 (Operational Land Imager, OLI)数据,通过采用降尺度模型,提供了基于modis的蒸散发(ET)从原来的500 m空间分辨率降尺度到30 m空间分辨率的建模解决方案。利用30 m空间分辨率的Lansat 8数据,计算了地表反照率、地表温度、归一化植被指数(NDVI)、土壤校正植被指数(SAVI)、改良土壤校正植被指数(MSAVI)、归一化建筑指数(NDBI)、归一化水分指数(NDWI)、归一化水分指数(NDMI)和7波段归一化红外指数(NDIIB7) 9个指数。建立多元线性回归(MLR)和最小二乘支持向量机(LS-SVM)模型,生成500 m尺度MODIS 500 m ET与Landsat指数之间的关系。此外,利用这些开发模型估算了基于30 m Landsat 8指数的30 m ET。采用相关系数(CC)、NASH - sutcliffe系数(NASH)效率、均方根误差(RMSE)和归一化均方误差(NMSE)对所开发模型(MLR和LS-SVM)的性能进行评估。采用Penman-Monteith (PM)方法,利用台站观测资料估算ET。结果表明:12月ETO最小,5月ETO最大;利用这些性能指标,发现LS-SVM模型的性能略优于MLR模型。然而,与Penman-Monteith方法相比,缩小模型高估了ET。各站MODIS ET与LS-SVM ET存在显著相关。
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引用次数: 1
Determining the influence of meteorological parameters on outdoor thermal comfort using ANFIS and ANN 应用ANFIS和ANN确定气象参数对室外热舒适性的影响
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.2976
Rishika Shah, RK Pandit, MK Gaur
The study aims to develop artificial neural networks for prediction of outdoor thermal comfort using meteorological parameters as input parameters. Universal Thermal Climate Index (UTCI) is used as the target parameter. For this purpose, a total number of 5088 hours of field monitoring data was considered from four representative urban streets of Gwalior city, India. First, linear association was determined between meteorological parameters. Mean radiant temperature was to be in high correlation with globe temperature and surface temperature. Second, Adaptive Neuro Fuzzy Inference System (ANFIS) was used to rank the meteorological parameters in order of their impact on UTCI. Air temperature was found to be having highest influence. Third, ANN models are developed to predict UTCI with air temperature as the only meteorological parameter in input layer. The developed ANN models for all four streets show remarkable predictive ability for both summer (R2 = 0.852, 0.986, 0.962, 0.955) and winter season (R2 = 0.976, 0.870, 0.941, 0.950). Additionally, the success index of the developed models is found to be in range 0.73 – 1, 0.88 – 1, 0.86 – 1, 0.87 – 1 for summer season and 0.78 – 0.99, 0.61 – 0.98, 0.55 – 0.98, 0.87 – 0.99 for winter season. The study contributes to the smart city initiatives for future urban designing by establishing that outdoor thermal comfort can be easily predicted using air temperature when other microclimatic parameters are difficult to record using machine learning approach. 
本研究旨在利用气象参数作为输入参数,开发用于预测室外热舒适度的人工神经网络。通用热气候指数(UTCI)被用作目标参数。为此,考虑了印度瓜廖尔市四条代表性城市街道共计5088小时的现场监测数据。首先,确定了气象参数之间的线性关联。平均辐射温度与地球温度和地表温度高度相关。其次,采用自适应神经模糊推理系统(ANFIS)对气象参数按其对UTCI的影响程度进行排序。空气温度的影响最大。第三,建立了以气温为输入层唯一气象参数的人工神经网络模型来预测UTCI。所开发的四条街道的人工神经网络模型对夏季(R2=0.852、0.986、0.962、0.955)和冬季(R2=0.976、0.870、0.941、0.950)都显示出显著的预测能力。此外,所开发的模型的成功指数在夏季为0.73-1、0.88-10.86-10.87-10.78-0.99、0.61-0.98,0.55-0.98,冬季为0.87–0.99。该研究通过确定当使用机器学习方法难以记录其他小气候参数时,可以使用空气温度轻松预测室外热舒适度,从而为未来城市设计的智能城市举措做出贡献。
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引用次数: 0
Cyclonic storms and depressions over the North Indian Ocean during 2022 2022 年期间北印度洋上空的气旋风暴和低气压
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.6295
Editor Mausam
During 2022, in all 15 cyclonic disturbances (CDs) formed over the Indian seas. These included; two severe cyclonic storms (ASANI & MANDOUS), one cyclonic storm (SITRANG), four deep depressions, six depressions and two land depressions. Out of these 15 CDs, ten formed over the Bay of Bengal (BoB), three over the Arabian Sea (AS) and two over land. One severe cyclonic storm, one deep depression and two depressions formed over BoB in pre-monsoon season. Monsoon season witnessed development of one depression and one deep depression over the BoB, two land depressions and two depressions over the AS. During the post monsoon season, one severe cyclonic storm, one cyclonic storm & two depressions formed over the BoB and one deep depression over the AS.
2022 年期间,印度海域共形成了 15 个气旋性扰动(CDs)。其中包括两个强气旋风暴(ASANI 和 MANDOUS)、一个气旋风暴(SITRANG)、四个深低压、六个低压和两个陆地低压。在这 15 个气旋风暴中,10 个在孟加拉湾(BoB)上空形成,3 个在阿拉伯海(AS)上空形成,2 个在陆地上空形成。在季风季节前期,孟加拉湾上空形成了一个强气旋风暴、一个深低压和两个低气压。季风季节,BoB 上形成了一个低气压和一个深低气压,AS 上形成了两个陆地低气压和两个低气压。后季风季节期间,在波罗的海上空形成了一个强气旋风暴、一个气旋风暴和两个低气压,并在澳大利亚西部上空形成了一个深低气压。
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引用次数: 0
Trend assessment of rainfall, temperature and relative humidity using non-parametric tests in the national capital region, Delhi 使用非参数测试对国家首都地区德里的降雨、温度和相对湿度的趋势评估
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.4936
Jitendra Rajput, N. Kushwaha, D. Sena, DK Singh, I. Mani
Understanding rainfall and temperature’s spatio-temporal variations at the local, regional, and global scale is vital for planning soil and water conservation structures and making irrigation decisions. The present investigation attempts to observe the rainfall and temperature variability and trend over 31 years (1990-2020) in the National Capital Region (NCR), Delhi, India, obtained from IARI meteorological station, Pusa, New Delhi. The statistical trend analyses Mann-Kendall (MK) test followed by Theil Sen slope estimator test was used for annual and monthly analysis to assess the trend direction and magnitude of the change over time. Pettitt's test detected the inflection point in the variable time series. The annual Tmax, Tmin, and rainfall showed no trend in the time series data. However, Tmax indicated a statistically significant decreasing trend in January and December. This implies a dip in the temperature during the winter months of January and December. Similarly, Tmin revealed a statistically significant decreasing trend in January and December. But a statistically increasing trend for Tmin was observed in April, which may cause a harsh environment for cultivating the Zaid season crops due to increased warming. The Pettitt test showed no change point in the time series trend in the annual Tmax and Tmin data series. For January Tmax data, the trend change point occurred in 1998. However, it was observed that Tmin in April showed a change point in the time series trend in 1999. The change point in the annual average rainfall data was marked in 2012. A didactic implication of these changes on hydrologic design and crop irrigation decisions was discussed in this paper.
了解局地、区域和全球尺度上降雨和温度的时空变化对水土保持结构规划和灌溉决策至关重要。本文利用位于新德里普萨的IARI气象站的数据,对印度德里国家首都地区(NCR) 1990-2020年31年的降水和气温变化趋势进行了观测。采用统计趋势分析Mann-Kendall (MK)检验和Theil Sen斜率估计检验进行年度和月度分析,以评估随时间变化的趋势方向和幅度。Pettitt的检验检测了变量时间序列的拐点。年Tmax、Tmin和降雨量在时间序列数据中没有变化趋势。1月和12月Tmax呈显著下降趋势。这意味着在冬季的1月和12月气温会下降。同样,Tmin在1月和12月也呈现出统计学上显著的下降趋势。但统计数据显示,4月份Tmin呈上升趋势,这可能会导致气候变暖导致种植扎伊德季节作物的环境变得恶劣。Pettitt检验显示,年Tmax和Tmin数据序列在时间序列趋势上没有变化点。对于1月份的Tmax数据,趋势变化点出现在1998年。然而,4月份的Tmin在1999年的时间序列趋势中表现出一个变化点。年平均降雨量数据的变化点标注在2012年。本文讨论了这些变化对水文设计和作物灌溉决策的指导意义。
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引用次数: 0
Rainfall analysis over 31 years of Chintapalle, Visakhapatnam, High Altitude and Tribal zone, Andhra Pradesh, India 印度安得拉邦钦塔帕勒、维萨卡帕特南、高海拔和部落地区31年的降雨量分析
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.818
G. Rao, A. Sowjanya, D. Shekhar, BNSandeep Naik, Bvs Kiran
Climate change and variability, particularly which of the annual rainfall, has received a great deal of interest to researchers worldwide. The extent of the variability of rainfall varies according to locations. Consequently, investigating the dynamics of rainfall variable in the perspective of changing climate is important to evaluate the impact of climate change and adapt potential mitigation strategies. To gain insight, trend analysis has been employed to inspect and quantify the rainfall distribution in the Chintapalli, Visakhapatnam district of Andhra Pradesh, India. Thirty-one years for a period of 1990–2020 long historical rainfall data series for different temporal scales (Monthly, Seasonal and Annual) of the study region was used for the analysis. Statistical trend analysis techniques namely Mann–Kendall (MK) test was used to detect the trend. To compute trend magnitude, Theil–Sen approach (TSA) was used for calculation of Sen’s slope. The detailed analysis of the data for 31 years indicates positive increasing trend with 2.13mm per year derived from the linear regression. MK test detected that there were rising and falling trends for various time scales in the study area. Departure analysis of rainfall indicated that a possible chance of normal rainfall, more frequently in the area. Rainfall Anomaly Index (RAI) analysis revealed that normal for most of the years, however, 2002 is the very dry year. While last ten years, the frequency of drought occurrence is thrice, but the magnitude is low. The study results will help in persuading the rainfall risks with effective use of water resources which can increase crop productivity and likely to manage natural resources for sustainability at HAT zone of Andhra Pradesh.
气候变化和可变性,特别是年降雨量,引起了世界各地研究人员的极大兴趣。降雨量的变化程度因地点而异。因此,从气候变化的角度研究降雨变量的动态对于评估气候变化的影响和调整潜在的缓解策略非常重要。为了深入了解情况,已采用趋势分析来检查和量化印度安得拉邦维萨卡帕特南区Chintapalli的降雨量分布。研究区域不同时间尺度(月度、季节性和年度)的1990-2020年31年长历史降雨量数据系列用于分析。使用统计趋势分析技术,即Mann-Kendall(MK)检验来检测趋势。为了计算趋势幅度,使用泰尔-森方法(TSA)计算森的斜率。对31年数据的详细分析表明,线性回归得出的数据呈每年2.13毫米的正增长趋势。MK检验发现,研究区域内不同时间尺度存在上升和下降趋势。对降雨量的偏离分析表明,正常降雨的可能性较大,在该地区更频繁。降雨量异常指数(RAI)分析显示,大多数年份都是正常的,但2002年是非常干旱的一年。近十年来,干旱发生频率为三倍,但程度较低。研究结果将有助于说服有效利用水资源的降雨风险,这可以提高作物生产力,并有可能管理安得拉邦HAT地区的自然资源以实现可持续性。
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引用次数: 0
Modelling spatiotemporal tendencies of climate types by Markov chain approach : A case study in Sanliurfa province in the south-eastern of Turkey 用马尔可夫链方法模拟气候类型的时空趋势——以土耳其东南部Sanliurfa省为例
IF 0.6 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2023-07-03 DOI: 10.54302/mausam.v74i3.872
A. Keskiner, M. Cetin
Identification of spatiotemporal tendencies of climate types may help water managers mitigate the negative impacts of droughts on water-demanding sectors. The primary objective of this study was to figure out the spatiotemporal tendencies of climatetypes in Sanliurfa province by using Erinc’s aridity index (EDI). To that end, long-term (1965-2018) annual precipitation and average annual maximum temperature series of meteorological stations were obtained and utilized to calculate the EDI series on a yearly basis. The EDI series of each station was divided into three periods, non-overlapping and successive, i.e., P1 (1965-1981), P2 (1982-1999) and P3 (2000-2018). Outliers were detected, andremoved from the EDI series; missing data were completed by regression analysis. The Markov transition probability matrix of the climate classes for the three periods was estimated for each station. Maps of the initial probability vectors and steady-state probabilities for the three periods of each climate class were generated by the inverse distance-weighted technique. Hypsometric curves for each climate class, as well as period, were developed and areal coverage of occurrence probabilities (OP) was determined. Results indicated that, as time progressed, the areal extent of severe-arid and arid climatic classes continued consistently to spread from the south to the north. Areas of semi-arid climate type showed a slight tendency towards the arid-climate type. Construction of large dams in the region could not prevent the shifts in the climate in favour of developing arid zones. The humid climate class is likely to vanish away in the future. Research led us to conclude that the expansion of the aridzone from south to northhas been alarming in terms of the adequacy of water resources. It is strongly recommended that spatiotemporal climate change studies should be periodically conducted in tandem with forest management practices for the region.
识别气候类型的时空趋势可以帮助水资源管理者减轻干旱对需水部门的负面影响。本研究的主要目的是利用Erinc干旱指数(EDI)分析三流法省气候类型的时空变化趋势。为此,获取气象站长期(1965-2018)年降水量和年平均最高气温序列,并利用其计算年际EDI序列。各站的EDI序列划分为P1(1965-1981)、P2(1982-1999)和P3(2000-2018)三个不重叠且连续的时期。检测到异常值,并从EDI系列中删除;通过回归分析补齐缺失资料。估计了各台站三个时期气候类别的马尔可夫转移概率矩阵。每个气候类别的三个时期的初始概率向量和稳态概率图是通过逆距离加权技术生成的。建立了各气候类别和时期的等温曲线,并确定了发生概率(OP)的面积覆盖。结果表明,随着时间的推移,严重干旱和干旱气候等级的面积范围持续从南向北扩展。半干旱气候型地区向干旱气候型转变的趋势较弱。在该地区建造大型水坝并不能阻止气候向有利于发展干旱地区的方向转变。湿润气候类很可能在未来消失。研究使我们得出结论,就水资源的充足性而言,干旱区从南向北的扩张令人担忧。强烈建议将时空气候变化研究与该区域的森林管理做法结合起来定期进行。
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引用次数: 1
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