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主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

Table of Content

    28 June 2023, Volume 39 Issue 3 Previous Issue    Next Issue
    Articles
    Diagnostic analyses of heavy rainfalls caused by two similar northward- moving typhoons using moist potential vorticity
    Liang-chen MA,Ye HUO,Ning WANG,Qian LI,Yue-ming YU
    2023, 39 (3):  1-9.  doi: 10.3969/j.issn.1673-503X.2023.03.001
    Abstract ( 157 )   HTML ( 17 )   PDF (9999KB) ( 129 )   Save

    Using the ERA5 reanalysis data of August 28-29 in 2012 and September 7-8 in 2019 with a horizontal resolution of 0.25°×0.25°, ground observation data, and the China Meteorological Administration tropical cyclone optimal moving path data, the diagnosis and analysis of wet potential vorticity of two typhoons "Bolaven" and "Lingling" with similar moving path northward causing heavy rainfalls in Northeast China were carried out.The results show that the heavy rainfalls caused by typhoons correspond well with the dense zone of pseudo-equivalent potential temperature (θse), and the rainfall is mainly located on the warm side of the dense zone of θse.The stronger the front zone is, the greater the rainfall is.Both typhoon processes have convectively unstable stratification in the early rainfall period, which provides initial energy accumulation for typhoon rainfall.The wet symmetry instability at the initial moment is the main factor for the occurrence of heavy rainfall on the northwest side of the typhoon center.During the time of rainfall enhancement, the instability of atmospheric convection is involved again, indicating that the instability of low-level convection provides the main energy for the rapid enhancement of rainfall.The absolute values of the wet barotropic term (MPV1) and the wet baroclinic term (MPV2) in the lower layer experienced an increase first, followed by decrease, and then changing to increase again, and the heavy rainfall mainly distributes in the intermediate period of the two extreme values.The rainstorm belts in central Jilin province caused by the two northward typhoons have a good correspondence with the negative MPV2 and positive MPV1 areas at the lower level of 850 hPa.

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    Characteristics and physical condition analyses of a supercell tornado in the Suihua area in 2020
    Ying-xu WU,Yi ZHOU,Ning ZHAO,Chen LUAN,Li-bao ZHANG,Mei-ling ZHAO,Kang-long CAI,Guang-na ZHAO
    2023, 39 (3):  10-19.  doi: 10.3969/j.issn.1673-503X.2023.03.002
    Abstract ( 94 )   HTML ( 9 )   PDF (6953KB) ( 67 )   Save

    Using the conventional data, regional automatic station data, FY-4 satellite cloud image, a new generation weather radar, and the ECMWF reanalysis data, the structural characteristics, formation process, and trigger mechanism of EF2 tornado in Suisheng Manchu town of Suihua city in Heilongjiang province on August 9, 2020, were analyzed.The results show that the tornado occurs under the background of the southwest airflow at 500 hPa in the front of the northeast cold vortex bottom, the warm shear line in the lower level, and the warm front on the ground.The dry transport in the middle layer is conducive to the sinking airflow, the warm and wet airflow in the lower layer and the divergence in the upper layer strengthen the rise of the airflow, and the enhanced horizontal vorticity forms a vortex tube under the action of strong vertical wind shear in the lower layer, providing favorable environmental conditions for the occurrence of tornadoes.The smaller the temperature lapse rate in the lower layer, the larger the convection suppression energy and the two convergence lines on the ground trigger the formation of supercells together.Different from previous tornado processes in Heilongjiang province, the convective effective potential energy of this tornado weather is low, the convective suppression energy is large, and there is no mainline trigger.The medium intensity and deep mesocyclone develops from 0.5° elevation to the middle level and strengthens, and the maintenance time is about 50 minutes.When the rotation speed of the mesocyclone in the middle level exceeded that of the low level, the tornado is generated.

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    Numerical simulation of a strong convective lightning process in Hainan island with different lightning parameterization schemes
    Wei YANG,Xun LI,Jian-xing LIN,You-long CHEN,Bin-yu YANG
    2023, 39 (3):  20-30.  doi: 10.3969/j.issn.1673-503X.2023.03.003
    Abstract ( 60 )   HTML ( 11 )   PDF (6108KB) ( 112 )   Save

    The WRF V3.9.1 mesoscale model coupled with the non-inductive electrification scheme and the lightning parameterization scheme was used to simulate a strong convection process occurred in Hainan Island on June 26, 2018.The simulation ability of lightning activity in tropical islands was discussed using three lightning parameterization schemes (LPI scheme, PR92w scheme, PR92z scheme) in the model.The results show that the model can well reproduce the radar echo characteristics of the strong convective process, the vertical velocity and hydrometeor particles are important factors affecting the model prediction of lightning, and the strong vertical velocity and abundant ice particles in the cloud are conducive to the development of the electric process in the cloud.LPI and PR92w schemes reproduce the distribution pattern of lightning and the structure of positive and negative lightning with an electric charge area between 8~15 km, while the lightning simulated by the PR92z scheme shows a scattering pattern, with a large deviation.The Equitable Threat Score (ETS) of the LPI scheme is the best with a value of 0.65.Further analysis of the correlation between LPI and lightning frequency shows that there is a significant positive correlation between them.The correlation coefficient between the regional average LPI and lightning frequency is 0.9, and the goodness of fitting value is 0.83.

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    Application of the SAL method to test the precipitation forecast of typhoons in Northeast China
    Xiao-tong ZHU,Kai YAO,Shang-feng LI,Mei-hui QU
    2023, 39 (3):  31-39.  doi: 10.3969/j.issn.1673-503X.2023.03.004
    Abstract ( 151 )   HTML ( 12 )   PDF (5114KB) ( 46 )   Save

    The strongest precipitation days of three north-moving typhoons affecting Northeast China in 2020 were selected as examples, the best method was used to determine the threshold and identify the precipitation subjects and individuals, and the SAL (structure, amplitude and location) test was carried out to analyze and evaluate the effects of 12-36 h forecast of the China Meteorological Administration's Global Generalized Forecast System (CMA-GFS), European Center for Medium-Range Weather Prediction (EC) model and China Meteorological Administration Mesoscale Numerical Weather Prediction System (CMA-MESO) model on typhoon precipitation in Northeast China.The results show that the forecasting effect of CMA-GFS for the precipitation process of typhoon Bavi is the best.For Typhoon Mavsak, the precipitation process intensity forecasted by the CMA-MESO model is stronger than those of the other two models.The structure forecast by the CMA-GFS model is better, and the precipitation position forecasted by the EC model is the best.The CMA-GFS and EC models are better at predicting the intensity of the precipitation process of Typhoon Haishen, and the EC model is the worst at predicting the structure but the best at predicting the precipitation location.We test and analyze three typhoon models affecting Northeast China in 2020 to explore preliminarily the forecast tendency of each model in typhoon forecast.In the forecast of typhoon precipitation intensity in Northeast China in the future, especially when similar typhoons occur, selective reference and purposefully subjective correction can be operated according to the model forecast characteristics.

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    Prediction and evaluation of short-term heavy precipitation around the Bohai Sea by a regional model based on the neighborhood method
    Xu-xuan JIA,Li-peng ZHANG,Sai-di WANG,Tian-jiao ZHOU,Jun LIANG
    2023, 39 (3):  40-46.  doi: 10.3969/j.issn.1673-503X.2023.03.005
    Abstract ( 112 )   HTML ( 7 )   PDF (1753KB) ( 97 )   Save

    Using Grapes_3km, mesoscale regional model precipitation forecast data over East, North, and Northeast China and 1 h precipitation data set of Land surface Data assimilation System of China Meteorological Administration (CLDAS) from May to September of 2020, the short-term heavy precipitation forecast (≥20 mm·h-1) around the Bohai Sea under the influence system of 850 hPa shear line outside the subtropical high, Northeast Cold Vortex, 500 hPa upper trough, typhoon, 500 hPa upper trough outside typhoon and 850 hPa shear line was tested and evaluated based on the neighborhood method.The results show that the FSS (fractions skill score) and hit ratio of each regional model are very low in the forecast of short-term heavy precipitation around the Bohai Sea when the neighborhood is 5 km.With the increase of the neighborhood, the test results give the score results that are valuable when there is displacement deviation in the forecast starting from the 50 km neighborhood.Grapes_3km and East China regional model FSS receives the minimum forecast skills in the 250 km and 300 km neighborhood, respectively, for the short-time heavy precipitation under the Category 5 influence system, whereas the other regional models do not receive the minimum forecast skills in the neighborhood.For the short-time heavy precipitation under other affected systems, the FSS of the four models in each neighborhood does not receive the minimum prediction skill, and the FSS of the North China model for the type 2, 3, and 4 affected systems is higher than that of the other models.The FSS of Grapes_3km for the type 1 affected system is higher than that of the other models.According to the test results of hit and false alarm ratios, Grapes_3km, the North China model and the East China model have better prediction effects for short-term heavy precipitation under type 1, 3, and 5 influence systems, type 2, 3, and 4 influence systems, and type 5 influence systems, respectively.

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    Visibility characteristics and influencing factors of a fog-haze process in Qingdao
    Wen-li LÜ,Xiao-meng SHI,Kai ZHANG
    2023, 39 (3):  47-55.  doi: 10.3969/j.issn.1673-503X.2023.03.006
    Abstract ( 113 )   HTML ( 18 )   PDF (3316KB) ( 150 )   Save

    Taking Qingdao as an area of concern, this paper analyzes the dynamic change characteristics and influencing factors of visibility during the fog-haze process using meteorological data including visibility at Qingdao, Pingdu, Huangdao and Jiaozhou stations and observation data such as PM2.5 concentration and water-soluble ion concentration at nearby environmental monitoring stations from November 16 to 20, 2021.The results show that the whole haze process in Qingdao from November 16 to 20, 2021 experienced the transitions of light fog, dry haze, wet haze, dry haze, wet haze, dry haze, wet haze, and light fog.Geographical discrepancies make the inland stations experience no light fog stage and the haze stage starting 8 hours earlier than the coastal stations.In the fog and haze process, the atmosphere appears stable junction and a certain humidity condition with the ground wind speed being less than 2 m·s-1 and the vertical movement speed being 0.0~0.5 Pa·s-1.The large amount of water vapor carried by the easterly wind and the variation of humidity layer above 80% are significant factors for the transition between dry and wet haze.Visibility gradually decreases with the enhancement of PM2.5 concentration and relative humidity.When the relative humidity increases, the correlation between visibility and PM2.5 concentration decreases.Compared with the dry haze stage, the PM2.5 concentration in wet haze increases by 14.1%, visibility decreases by 47.4%, and visibility decreases by 7.6% after the transition from haze to fog.In the dry haze stage, visibility is significantly affected by the PM2.5 level.In the wet haze stage visibility is affected by both PM2.5 level and relative humidity, whereas in the fog phase visibility is significantly affected by relative humidity.In the haze stage, the SNA concentration (SO42-, NO3-, NH4+), SOR (sulfur oxidation rate), and liquid water content in particulate matter gradually increase with the enhancement of pollution level leading to visibility gradually decreasing.The backward trajectories indicate that during the haze period, the air masses originate from inland, passing through Jiangsu provrce, He'nan provice, and other places to Qingdao with a deep pollution degree, while during the fog period, the air masses reach Qingdao through the coastal areas with high humidity and low pollution degree.

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    Influencing factors and pollutant characteristics of radiation fog in the Beijing-Tianjin-Hebei region
    Min XU,Jiang-bo LI,Xiao-fei TIAN,Rui-fang ZHANG,Fang SHEN,Zhang-yan LE
    2023, 39 (3):  56-64.  doi: 10.3969/j.issn.1673-503X.2023.03.007
    Abstract ( 103 )   HTML ( 7 )   PDF (3513KB) ( 114 )   Save

    Based on the surface and upper air meteorological data and air quality data in the Beijing-Tianjin-Hebei region, the climatic characteristics of radiation fog and the variations of influence factors and particle pollutants of various scales before and after the occurrence of radiation fog from 2000 to 2020 were analyzed.The results show that the radiation fog occurs frequently in the central and southern plains of the Beijing-Tianjin-Hebei region, whereas such a fog rarely occurs in the Bashang plateau and the mountainous area in the northwest of Beijing.The minimum visibility of radiation fog generally decreases to 0.1~0.6 km and increases significantly with the sunrise.The high-low temperature differences, i.e.the differences between the maximum temperature on the day before the occurrence of radiation fog and the minimum temperature of the radiation fog day are concentrated between 6.0 ℃ and 10.4 ℃, with the maximum up to 20.3 ℃, and the minimum is 0 ℃ and the value varies significantly in different regions.The high-low temperature differences in spring appear larger than those in other seasons, but the maximum and minimum differences appear in winter.At 14:00 on the day before the occurrence of radiation fog, the surface wind speed is mostly varying from 1.0~2.4 m·s-1, whereas at 20:00 and 08:00 on the fog day, the wind speed decreases to around 1.0 m·s-1, with the wind direction of north and south.Vertical inverses tend to start at ground level and usually appear shallow, with wind direction shifting counterclockwise from north to west with height.On the day when the fog breaks out, the temperature and wind speed increase whereas the humidity decreases with sunrise, and PM2.5 and PM10 level decrease, resulting in the air pollution level gradually decreasing.

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    Comparison of automatic and artificial acid rain observation data in Shanxi province
    Ya-jun LI,Xia CAI,Xun ZHANG,Qian-qian WEI,Li-li GE,Rui-jie SU
    2023, 39 (3):  65-71.  doi: 10.3969/j.issn.1673-503X.2023.03.008
    Abstract ( 57 )   HTML ( 2 )   PDF (1766KB) ( 104 )   Save

    The pH and conductivity data measured automatically and artificially from five acid rain observation stations in Shanxi province were analyzed to evaluate the discrepancy between the two observation methods.The results show that the precipitation sampling of the five stations is normal during parallel observation, the missing rate of automatic observation is 3.6%, and the trouble-free operation time of the instrument reaches 99.0%.In terms of pH measurement, 86.9% of non-acid rain (pH>5.6) was observed artificially during the study, which was lower than that of automatic observation (91.5%).The proportion of observation times with the relative pH deviation of manual and automatic observation values within 20% was 91.25%.For the measurement of the conductivity K value, the number of observations with a deviation between the two methods within 20% accounted for 64.1%.The linear correlation between artificial and automatic measurements of electrical conductivity at the five observation stations is significantly higher than that of pH.In general, the operation of the instrument is relatively reliable, but there are still some discrepancies between the artificial and automatic observations during parallel observation.Therefore it is recommended to extend the parallel observation time.

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    Spatial-temporal characteristics of low visibility in Tianjin and its application in expressway meteorological service
    Li-yuan REN,Ming-ming XIONG,Mei-ling SUN,Xue-jiao WANG
    2023, 39 (3):  72-78.  doi: 10.3969/j.issn.1673-503X.2023.03.009
    Abstract ( 90 )   HTML ( 11 )   PDF (1562KB) ( 252 )   Save

    Based on the visibility and precipitation observation data from traffic automatic weather stations, national ground meteorological observation stations, and some regional automatic weather stations in Tianjin from 2017 to 2020, the spatial-temporal variation characteristics of low visibility which has a great impact on expressway traffic safety and their relationships with precipitation were analyzed.The risk level of low visibility and corresponding key service period of each expressway were provided.The results show that the number of low visibility days in Tianjin has an annual mean value of 22.1 days and indicates an obvious spatial variability with the highest value in the north, followed by the west and south, and the least in the east.Low visibility is mostly concentrated from September to February of the next year, and the frequency is higher in nighttime than in daytime, usually reaching the maximum around 06:00.Summer precipitation has a significant impact on low visibility, and low visibility affected by precipitation accounts for about 47.1% of the total from July to August, and mainly occurs during 13:00-15:00 and 19:00-08:00.The expressways with higher risk of the low visibility account for about 57.1% of all.There are also significant differences in the concerned sections and key service periods among different expressways.

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    Analysis of city effect of precipitation in Harbin based on the backbone station network
    Heng-yuan KANG,Yu-lian LIU,Fang YUAN,He-ling ZHOU
    2023, 39 (3):  79-86.  doi: 10.3969/j.issn.1673-503X.2023.03.010
    Abstract ( 47 )   HTML ( 5 )   PDF (1360KB) ( 47 )   Save

    Based on the hourly monitoring data of the meteorological backbone automatic stations in Harbin from 2018 to 2021, this paper analyzed the impact of the city on summer precipitation.Results showed that: the heat island intensity in Harbin is 0.79℃ on average in summer with a daily variation that is stronger at night and weaker in daytime.The temperature difference is the largest in the eastern suburbs and the smallest in the northern suburbs.The most and least precipitation in summer is respectively distributed in the eastern suburbs on the downwind side and the southern suburbs on the upwind side in Harbin.The hourly precipitation probability is higher in suburbs than in urban areas, and many precipitations occurring in the afternoon and early morning for the former are respectively delayed and advanced relative to these for the latter.The precipitation probability is greater in urban areas during the daytime and in suburbs at night.The difference of precipitation between daytime and nightime in the northern suburbs is the largest.The maximum hourly precipitation in the suburbs is greater than that in the urban areas.The hourly precipitation intensity in the urban area and the eastern suburbs is larger than in the southern and northern suburbs.Short-duration rainfall in Harbin′s is more frequent and has a greater contribution rate.The precipitation lasting within 6 hours appears most frequently in urban areas, and rarely in the northern suburbs, and that lasting for 6-12 hours appears rarely in urban areas and most frequently in the eastern suburbs, while that beyond 12 hours occurs most frequently in the northern suburbs, and shows the highest contribution rate in the southern suburbs.

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    Analysis of low-level jets during heavy snowfalls in Jinzhou
    Cui-yan ZHANG,Shu-ting CHANG,Zi-yi QU,Miao WANG,Jiao-yang WANG,Jun LIANG
    2023, 39 (3):  87-96.  doi: 10.3969/j.issn.1673-503X.2023.03.011
    Abstract ( 109 )   HTML ( 5 )   PDF (6904KB) ( 51 )   Save

    Meteorological observation data and EC reanalysis data were used to analyze the climatic characteristics of heavy snowfalls (24-hour snowfall ≥ 5 mm)in Jinzhou during 2005-2021 and the variations of low-level jets during occurrence and development period of snowfalls under different weather patterns were compared.The results showed that heavy snowfall appears annually from November to March next year with an annual mean occurrence number of 1.6 times and happens most frequently in November and does not appear in January in Jinzhou and occurs more often in the north and south parts and lower infrequently in the central part of Jinzhou.Weather systems of heavy snowfall in Jinzhou are the northward Huabei (11.1%) and Jianghuai cyclone (51.9%) and the eastward Mongolia cyclone (37.0%).Under different weather situations, water resource and energy offered by low-level jets is the key to the occurrence of heavy snowfall.The wind speed of the low-level jet of the eastward Mongolia cyclone is the largest i.e.20 m·s-1, followed by the Huabei cyclone at 14 m·s-1 and the Jianghuai cyclone at 12 m·s-1.The area of the low-level jet of the Mongolia cyclone is the largest, followed by the Jianghuai cyclone and that of the Huabei cyclone is the smallest.Six hours before the snow falls, the low-level jets are all formed, including 96% of southward or southwestward jets and 4% of eastward jets.Two hours before snowfall, low-level jets are maintained and enlarge the impact range, and the vertical rising speed of airflow is(-1.0~-0.5)×10-3 Pa·s-1, which can be regarded as the indicator of the beginning of snowfall.During snowfall, the low-level jet at 800~900 hPa emerges, and there is a zone where wind speed is larger than 20 m·s-1 at 650~850 hPa, the vertical rising speed of airflow at the lower troposphere is increased to(-1.5~-1.0)×10-3 hPa·s-1, maintaining and intensifying the snowfall.

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    Analysis of the characteristics of local wind in the Three Gorges Reservoir area
    Qu GUO,Yong WANG,Rui LI,Tian-yu ZHANG,Zu-heng HU,Fen ZHANG
    2023, 39 (3):  97-105.  doi: 10.3969/j.issn.1673-503X.2023.03.012
    Abstract ( 59 )   HTML ( 3 )   PDF (3242KB) ( 47 )   Save

    Using the hourly data of five heights (10, 30, 50, 70, and 100 m) observed by the 100-meter wind tower at Muhe in the Fuling district, Chongqing in the Three Gorges Reservoir area, belonging to the local climate monitoring subsystem in ecology and environment monitoring network of the Yangtze River Three Gorges project, from 2010 to 2020, the characteristics of vertical change of local wind were analyzed.The results show that the wind speed at the same height is the biggest in spring and the smallest in winter, and shows a typical diurnal variation of the single peak type, reaching a bottom at about 9 o′clock and a peak at about 16 o′clock.The wind speed at 30~100 m height is almost the same during 10-13 o′clock in summer.The local wind direction is mainly influenced by the local terrain.The frequency of local wind direction along(SSW~ENE)the Yangtze River Valley at different heights ranges between 46% and 66%.When there is rainfall, the vertical difference of wind speed with the order from large to small is torrential rain, heavy rain, moderate rain, and light rain, respectively, and the vertical gradient of wind speed increases with the temperature increasing.When there is temperature inversion at night, the wind speed at 50 m height is smaller than that at 30 m height.

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    Effects of drought degree and nitrogen application level on leaf C and N contents and C/N ratio of spring maize
    Ni-na CHEN,Hui-jie LÜ,Yi-rui ZHANG,Guo-hui LI,Na MI,Shu-jie ZHANG,Si-yu LI,Yu-shu ZHANG
    2023, 39 (3):  106-116.  doi: 10.3969/j.issn.1673-503X.2023.03.013
    Abstract ( 66 )   HTML ( 2 )   PDF (1237KB) ( 92 )   Save

    To explore the effects of drought and nitrogen application on leaf C, N content, and C/N ratio of spring maize, "Danyu 405" was used as the test material.Comparative experiments of moderate (relative humidity is 45%±5%) and severe (relative humidity is 35%±5%) drought stress and nitrogen addition of 120 kg·hm-2, 240 kg·hm-2, and 270 kg·hm-2 were carried out to analyze the leaf C, N content and C/N ratio of maize under drought, nitrogen addition and their interactions in the three key developmental stages of maize during 2018 to 2019.The results indicated that drought caused a decrease of 3.3%~38.5% in leaf N content and an increase of 0.8%~67.1% in the C/N ratio.The effects on leaf C and N contents and C/N ratio at different growing stages are Milk maturity stage> tasselling stage > jointing stage.With the aggravation of drought, the effects of drought on leaf N content and C/N ratio are intensified.After N application, the leaf N content increases first and then decreases with the increase of N application, but the C/N ratio is opposite.When the nitrogen application rate is 120 kg·hm-2, the highest total nitrogen content and the lowest C/N ratio are obtained.A certain amount of nitrogen fertilizer after a drought can alleviate the negative effects of drought on the leaf carbon and nitrogen balance, but could not recover completely.When the nitrogen rate is 120 kg·hm-2, the recovery degree of leaf N content and C/N ratio are the most obvious, increasing by 11.2% and decreasing by 6.5% respectively.After rewetting, nitrogen application can not restore the C/N balance of drought-affected leaves to the control level.There is a significant linear negative correlation between maize yield and leaf total carbon content and C/N ratio and a significant linear positive correlation between maize yield and leaf total nitrogen content (P < 0.01).Different degrees of drought and nitrogen application levels can affect maize yield by affecting the content of carbon and nitrogen in maize leaves and the ratio of carbon to nitrogen.This study can provide a theoretical basis for maize growth monitoring and dryland agricultural production.

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    Study on the meteorological index of suitable sowing time of Isatis tinctoria in Heilongjiang province
    Nong CHEN,You-fang ZHANG,Xiang-ling YUAN,Min-hui YAN,Jing ZHANG,Jin-feng ZHANG,Ling GAO,Peng-yu YUAN
    2023, 39 (3):  117-123.  doi: 10.3969/j.issn.1673-503X.2023.03.014
    Abstract ( 56 )   HTML ( 7 )   PDF (1490KB) ( 237 )   Save

    In order to provide a scientific basis for the planting of Isatis tinctoria in Heilongjiang province, based on the daily soil temperature and precipitation data from 84 observations in Heilongjiang province from 1991 to 2020, using the 5-day sliding average method, 3-day sliding average method, Krikin interpolation method, mathematical-statistical analysis method, and hierarchical analysis method, the suitability of meteorological conditions at sowing stage of Isatis tinctoria and the effects of sowing at different temperature conditions on yield and active ingredient content of Isatis tinctoria were discussed.The results showed that the optimum sowing time was 12 ℃ with a daily average temperature of 5 cm.The first day of the 5 cm below-ground temperature stable passing 12 ℃ in Heilongjiang province is from May 1 to 30, and its spatial distribution shows a trend of a gradual delay from south to north and from plain to mountain.The general trend is that the first day appeared earlier in Dumeng, Tailai, Gannan, Zhaoyuan, and Wuchang, while the first day appeared later in Mohe, Huzhong, Xinlin, Tahe, Wuyiling, Jiayin, and Suifenhe.

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    Relationship between fruit cracking and indoor microclimate factors of watermelon during the expansion stage in Changle greenhouse
    Shu-jun LI,Jun-xian TANG,Hua ZHAO,Jing YUAN,Ai-ling ZHANG,Pei-juan WANG
    2023, 39 (3):  124-131.  doi: 10.3969/j.issn.1673-503X.2023.03.015
    Abstract ( 46 )   HTML ( 0 )   PDF (2448KB) ( 127 )   Save

    Using the greenhouse microclimate data and fruit cracking data of watermelon during the expansion stage, considering the meteorological conditions suitable for watermelon growth, 10 climate factors related to temperature and humidity were selected, the leading climate factors with high correlation with the number of fruit cracking were screened based on Pearson correlation analysis.The relationship between the fruit cracking of watermelon during the expansion stage of the greenhouse and indoor microclimate factors was analyzed.The results showed that there was a significant negative correlation between the number of cracked watermelons and the minimum temperature at night and a positive correlation between the number of cracked watermelons and the hourly maximum humidity difference at night.The goodness of fit (R2) of the climate regression equation of cracked watermelon during the expansion stage in the greenhouse reached 0.404, and the root mean square error (RMSE) between the simulated and actual number of fruit cracking in the verified sample is 6.8.The results show that the difference between minimum temperature and maximum hourly humidity at night could be used to simulate the cracked watermelon disaster in the greenhouse.

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    Variation characteristics of hydrothermal conditions for timely sowing of maize in Jilin province from 1981 to 2018
    Dong-ni WANG,Mei-yu WANG,Jing-quan REN,Qiao GUO,Jun-wei LI
    2023, 39 (3):  132-139.  doi: 10.3969/j.issn.1673-503X.2023.03.016
    Abstract ( 72 )   HTML ( 7 )   PDF (1137KB) ( 194 )   Save

    Based on the spring daily meteorological data of 50 meteorological stations and the development period data of 19 maize stations in Jilin province from 1981 to 2018, the spatial and temporal characteristics of the first saturating rain and the first day of temperature stable passing through 8 ℃ in spring and their effects on the timely sowing of maize were analyzed by using the method of agricultural climate statistics.The results showed that the average occurrence date of the first saturating rain generally showed a trend of early in the east and late in the west, with a difference of 20 d between the earliest and the latest.There is a difference of 35~52 days between the earliest and the latest years of the first saturating rain in the three climate zones.The difference between the earliest and the latest year when the temperature stable passes through 8 ℃ under an 80% guarantee rate is 28~31 d.The difference in spatial and temporal distribution of water and heat conditions is an important factor that causes the difference in maize planting time and seedling situation between years.The timely sowing of maize in the west is mainly affected by the presence or absence of saturating rain and the time of occurrence of saturating rain, in the middle is mainly affected by the time of occurrence of saturating rain, and in the east is mainly affected by temperature conditions.Only by combining agroclimatic and agrometeorological methods, can the suitable sowing date of the current year be better determined.

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    Review
    Review on three-dimensional monitoring and research progress on air pollution in urban agglomerations of Northeast China
    Xiao-lan LI,Yan-jun MA,Yang-feng WANG,Hu-jia ZHAO,Ye HONG,Ning-wei LIU,Yun-hai ZHANG
    2023, 39 (3):  140-153.  doi: 10.3969/j.issn.1673-503X.2023.03.017
    Abstract ( 57 )   HTML ( 6 )   PDF (7177KB) ( 55 )   Save

    Based on the project achievements of the National Key R & D Program of China "Three-dimensional monitoring technology system for combined air pollution in Harbin-Changchun Urban Agglomeration", this paper reviewed the main processes of the three-dimensional observation, characteristics, and formation mechanism of air pollution in urban agglomerations of Northeast China in recent years.We introduced the distribution and development of a monitoring network of air pollution in this region, summarized the spatiotemporal characteristics of air pollutants, optical properties, and chemical composition of aerosols, and analyzed the structure and physical process of planetary boundary layer and their impact on the formation and evolution of air pollution.Finally, we pointed out that it still needs to strengthen the research on the joint control of PM2.5 and ozone pollution and the impact of aerosol-PBL interaction mechanism on air pollution in urban agglomerations in Northeast China.

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    Bulletins
    Study on precipitation characteristics of Beijing municipal administrative center suitable for sponge city planning and construction
    Ruo-zi YANG,Chun-yi XUAN,Ji WANG,Wu-peng DU,Hua WANG
    2023, 39 (3):  154-160.  doi: 10.3969/j.issn.1673-503X.2023.03.018
    Abstract ( 45 )   HTML ( 2 )   PDF (2006KB) ( 17 )   Save

    Based on precipitation data from the meteorological observation stations, the temporal and spatial variation characteristics of daily precipitation in the area where the Beijing municipal administrative center is located were analyzed.The short duration rainstorm intensity formula suitable for Beijing municipal administrative center was compiled.Finally, the control target index for the construction of a sponge city in the sub-center, the total annual runoff control rate, was calculated.The results show that the annual variation of precipitation in the research area is large, the difference between the maximum precipitation and the minimum precipitation can reach 684.0 mm, and the annual precipitation distribution is uneven.The precipitation from June to September during the flood season (415.3 mm) accounts for 75% of the total precipitation in the whole year.The diurnal variation of precipitation, intensity, and frequency during flood season is a single peak pattern, and the distribution characteristics of precipitation and precipitation intensity are consistent.The main peak value appears at 22:00, the main valley value is at noon, the main peak value of precipitation frequency appears at 04:00, and the main valley value appears at 14:00.The multi-year variation trend of precipitation and intensity is consistent at most times, showing the characteristics of increasing and strengthening in the early morning and afternoon, and decreasing and weakening in the morning, noon and night.In terms of spatial distribution, most of the precipitation peaks in the north of the Beijing municipal administrative center occur at night, and most of the precipitation peaks in the south occur in the early morning.Comparing the results of the new rainstorm intensity formula with the current one, we can conclude that the larger the return period, the greater the precipitation intensity corresponding to the new formula.The new formula is more suitable for the design and construction of a sponge city under the background of frequent extreme precipitation in the future.When the control index of sponge city construction, the total annual runoff control rate, is 80% and 85%, the corresponding designed precipitation is 27.6 mm and 33.9 mm.

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    Seamless mosaic true color image processing method for FY-3D/MERSI-Ⅱ data
    Quan-jun HE,Yue-wei ZHANG
    2023, 39 (3):  161-168.  doi: 10.3969/j.issn.1673-503X.2023.03.019
    Abstract ( 81 )   HTML ( 6 )   PDF (6109KB) ( 118 )   Save

    A wide true color image processing method was proposed for the second generational medium resolution spectrum imager (MERSI-Ⅱ) on board the Chinese Fengyun-3D (FY-3D) polar orbit meteorological satellite.Using this method, the true color-composed image was realized by atmospheric correction and segmented enhancement for the three 250 m resolution visible bands of MERSI-Ⅱ.Then the seamless mosaic of multi-track images was realized based on pixel weighted fusion method and Wallis dodging algorithm.The application cases show that this method can obtain high-quality and intuitive remote sensing monitoring images, and effectively solve the limitation of scanning width of polar-orbit meteorological satellite's single-track data.This method is helpful to use polar orbit satellite data in monitoring services during emergency response.

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