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1.
渭北春玉米抑蒸集水防旱抗旱综合技术研究   总被引:1,自引:0,他引:1  
本试验开展了6种抑蒸集水综合抗旱技术田间试验。试验结果表明, 以地膜+ 垄植+ 中国旱地龙处理抑蒸集水和增产效果显著。水分利用效率达19.89kg/ (m m ·hm 2), 耗水系数仅0.05 m m / (kg·hm 2), 产量达7200 kg/hm 2, 比其它综合技术增产17% ~60% 。  相似文献   

2.
1990~1993年在渭北陇东黄土高原布置了晚播回荐麦一膜两用的田间试验,分析试验结果得:晚播回荐小麦覆膜,增温保墒效应明显,可提高地温2~4℃,节水30mm以上,促进了作物早发,保证了小麦安全越冬,比单作回荐麦增产53.0%,小麦返青揭膜覆于相邻作物带,做到一膜两用,集水调水效应显著,协调了不同作物需水的供需平衡,带田总产8212.5~9125.0kg/hm^2,比单作增产45%~166%。  相似文献   

3.
实施旱作小麦-玉米地膜带田种值,节水调水效应显著。覆膜田比不覆膜田1m土内层含水量多40~70mm,蒸散少30~50mm;作物相互调水60~70%。一种作物单生期,基本上是两带降水一带用;作物共生期,两种作物相互调节用,协调平衡了对水分的供需矛盾,水分利用率增加到15kg/mm·hm2以上,比单作物增产45%以上。  相似文献   

4.
仇化民  王宁珍  马妮娜 《气象》1995,21(2):51-54
旱作地膜小麦-玉米带田一膜两用技术热效应显著,可提高地温2—6℃,保证了小麦安全越冬,促进了作物早发;热资源利用率高达0.977,比单作提高了25%-40%;变作物一年一熟为一年两熟,亩产可达到440—610kg,比单作增产20%-80%.  相似文献   

5.
甘肃东部旱作区小麦产量变幅大,不分生产力变化极不稳定,但潜力很大。冬小麦降水和土壤水分生产力平均为0.92kg/mm和0.85g/mm和0.75kg/mm。土壤贮水量是旱作区小麦生产力的最重要因素。秋季土壤贮水量是翌年小麦产量的基础,有收无收的关键,对产量的贡献最大;小麦产量对春季土壤贮水量的利用率最高,对小麦高产优质至关重要。  相似文献   

6.
李玉林 《气象》1997,23(2):38-40
利用旬雨量与历史同期产量资料,使用积分回归和多元回归等方法,分析自然降雨量与水稻产量的关系,以证实人工增雨对水稻产量提高所起的作用。结果表明,全省早稻亩产量随旬雨量增加平均为0.164kg/mm,晚稻亩产量增加平均为0.11kg/mm。  相似文献   

7.
仇化民  王宁珍  马妮娜 《气象》1995,21(2):51-54
旱作地膜小麦-玉米带田-膜两用技术热效应显著,可提高地温2-6℃,保证了小麦安全越冬,促进了作物早发;热资源利用率高达0.977,比单作提高了25%-40%,变作物一年一熟为一年两熟,亩产可达到440-610kg,比单比增产20%-80%。  相似文献   

8.
全球农作物对大气CO2及其倍增的吸收量估算   总被引:15,自引:0,他引:15  
王修兰 《气象学报》1996,54(4):466-473
根据农作物产量资料(FAO1992年),计算出中国和全球各种作物对CO2的吸收总量分别为5.5×108t/aC和28.9×108t/aC。同时以不同CO2浓度下小麦、玉米、大豆等全生育期光合速率实验数据直接计算的C吸收量为对照,与相应的中国产量资料计算结果比较,两者相差2.6%。从而进一步依据作物对CO2倍增反应诊断实验结果,推算出大气CO2浓度比目前倍增(700ppm)条件下,中国和全球农作物吸收CO2总量将增长21%-26%,分别为6.6×108t/a—6.9×108t/a和34.1×108t/a—36.2×108t/aC。研究还表明,单位面积作物年吸C量全球(3.2t/(hm2·8))比中国(4.2t/(hm2·a))低25.4%,而且C4作物普遍高于同类C3作物。  相似文献   

9.
陈艳春  赵秀英 《气象》1996,22(11):44-48
分析了黄河三角洲地区主要栽培草种的气候生态适应性以及牧草生长季气候条件的优劣势。计算得出该区天然草场和人工草场的气候生产力、气候增产潜力,研究其时空分布规律,提出草场改良措施。结果表明:天然草场年气候生产力为9210—11820kg/ha。增产潜力为4500—10500kg/ha;种植紫花苜蓿的人工草场年气候生产力为23775—28080kg/ha,增产潜力为6000—19500kg/ha。  相似文献   

10.
前 言临夏州地处青藏高原东北侧边坡区,大部粮播区海拔高度为1800~2600m,年降水量为293.1~622.8mm,年平均气温为5.0~6.8℃,≥10℃持续日数为100~130d,积温为1400~2000℃,山区积温不足1400℃,属高寒阴湿区和干旱少雨区。春小麦是临夏州主产作物,每年播种达4.5~5.7hm2,占全州总粮播面积的33%~40%。高寒阴湿,热量不足,农业气象灾害多,是制约本地春小麦稳定增产的主要因素之一。为此,就临夏州地膜覆盖春小麦增温增产效应,进行了地温观测和对比试验。试验…  相似文献   

11.
The spatial and temporal variations of daily maximum temperature(Tmax), daily minimum temperature(Tmin), daily maximum precipitation(Pmax) and daily maximum wind speed(WSmax) were examined in China using Mann-Kendall test and linear regression method. The results indicated that for China as a whole, Tmax, Tmin and Pmax had significant increasing trends at rates of 0.15℃ per decade, 0.45℃ per decade and 0.58 mm per decade,respectively, while WSmax had decreased significantly at 1.18 m·s~(-1) per decade during 1959—2014. In all regions of China, Tmin increased and WSmax decreased significantly. Spatially, Tmax increased significantly at most of the stations in South China(SC), northwestern North China(NC), northeastern Northeast China(NEC), eastern Northwest China(NWC) and eastern Southwest China(SWC), and the increasing trends were significant in NC, SC, NWC and SWC on the regional average. Tmin increased significantly at most of the stations in China, with notable increase in NEC, northern and southeastern NC and northwestern and eastern NWC. Pmax showed no significant trend at most of the stations in China, and on the regional average it decreased significantly in NC but increased in SC, NWC and the mid-lower Yangtze River valley(YR). WSmax decreased significantly at the vast majority of stations in China, with remarkable decrease in northern NC, northern and central YR, central and southern SC and in parts of central NEC and western NWC. With global climate change and rapidly economic development, China has become more vulnerable to climatic extremes and meteorological disasters, so more strategies of mitigation and/or adaptation of climatic extremes,such as environmentally-friendly and low-cost energy production systems and the enhancement of engineering defense measures are necessary for government and social publics.  相似文献   

12.
Storms that occur at the Bay of Bengal (BoB) are of a bimodal pattern, which is different from that of the other sea areas. By using the NCEP, SST and JTWC data, the causes of the bimodal pattern storm activity of the BoB are diagnosed and analyzed in this paper. The result shows that the seasonal variation of general atmosphere circulation in East Asia has a regulating and controlling impact on the BoB storm activity, and the “bimodal period” of the storm activity corresponds exactly to the seasonal conversion period of atmospheric circulation. The minor wind speed of shear spring and autumn contributed to the storm, which was a crucial factor for the generation and occurrence of the “bimodal pattern” storm activity in the BoB. The analysis on sea surface temperature (SST) shows that the SSTs of all the year around in the BoB area meet the conditions required for the generation of tropical cyclones (TCs). However, the SSTs in the central area of the bay are higher than that of the surrounding areas in spring and autumn, which facilitates the occurrence of a “two-peak” storm activity pattern. The genesis potential index (GPI) quantifies and reflects the environmental conditions for the generation of the BoB storms. For GPI, the intense low-level vortex disturbance in the troposphere and high-humidity atmosphere are the sufficient conditions for storms, while large maximum wind velocity of the ground vortex radius and small vertical wind shear are the necessary conditions of storms.  相似文献   

13.
Observed daily precipitation data from the National Meteorological Observatory in Hainan province and daily data from the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis-2 dataset from 1981 to 2014 are used to analyze the relationship between Hainan extreme heavy rainfall processes in autumn (referred to as EHRPs) and 10–30 d low-frequency circulation. Based on the key low-frequency signals and the NCEP Climate Forecast System Version 2 (CFSv2) model forecasting products, a dynamical-statistical method is established for the extended-range forecast of EHRPs. The results suggest that EHRPs have a close relationship with the 10–30 d low-frequency oscillation of 850 hPa zonal wind over Hainan Island and to its north, and that they basically occur during the trough phase of the low-frequency oscillation of zonal wind. The latitudinal propagation of the low-frequency wave train in the middle-high latitudes and the meridional propagation of the low-frequency wave train along the coast of East Asia contribute to the ‘north high (cold), south low (warm)’ pattern near Hainan Island, which results in the zonal wind over Hainan Island and to its north reaching its trough, consequently leading to EHRPs. Considering the link between low-frequency circulation and EHRPs, a low-frequency wave train index (LWTI) is defined and adopted to forecast EHRPs by using NCEP CFSv2 forecasting products. EHRPs are predicted to occur during peak phases of LWTI with value larger than 1 for three or more consecutive forecast days. Hindcast experiments for EHRPs in 2015–2016 indicate that EHRPs can be predicted 8–24 d in advance, with an average period of validity of 16.7 d.  相似文献   

14.
Based on the measurements obtained at 64 national meteorological stations in the Beijing–Tianjin–Hebei (BTH) region between 1970 and 2013, the potential evapotranspiration (ET0) in this region was estimated using the Penman–Monteith equation and its sensitivity to maximum temperature (Tmax), minimum temperature (Tmin), wind speed (Vw), net radiation (Rn) and water vapor pressure (Pwv) was analyzed, respectively. The results are shown as follows. (1) The climatic elements in the BTH region underwent significant changes in the study period. Vw and Rn decreased significantly, whereas Tmin, Tmax and Pwv increased considerably. (2) In the BTH region, ET0 also exhibited a significant decreasing trend, and the sensitivity of ET0 to the climatic elements exhibited seasonal characteristics. Of all the climatic elements, ET0 was most sensitive to Pwv in the fall and winter and Rn in the spring and summer. On the annual scale, ET0 was most sensitive to Pwv, followed by Rn, Vw, Tmax and Tmin. In addition, the sensitivity coefficient of ET0 with respect to Pwv had a negative value for all the areas, indicating that increases in Pwv can prevent ET0 from increasing. (3) The sensitivity of ET0 to Tmin and Tmax was significantly lower than its sensitivity to other climatic elements. However, increases in temperature can lead to changes in Pwv and Rn. The temperature should be considered the key intrinsic climatic element that has caused the "evaporation paradox" phenomenon in the BTH region.  相似文献   

15.
正The Taal Volcano in Luzon is one of the most active and dangerous volcanoes of the Philippines. A recent eruption occurred on 12 January 2020(Fig. 1a), and this volcano is still active with the occurrence of volcanic earthquakes. The eruption has become a deep concern worldwide, not only for its damage on local society, but also for potential hazardous consequences on the Earth's climate and environment.  相似文献   

16.
The moving-window correlation analysis was applied to investigate the relationship between autumn Indian Ocean Dipole (IOD) events and the synchronous autumn precipitation in Huaxi region, based on the daily precipitation, sea surface temperature (SST) and atmospheric circulation data from 1960 to 2012. The correlation curves of IOD and the early modulation of Huaxi region’s autumn precipitation indicated a mutational site appeared in the 1970s. During 1960 to 1979, when the IOD was in positive phase in autumn, the circulations changed from a “W” shape to an ”M” shape at 500 hPa in Asia middle-high latitude region. Cold flux got into the Sichuan province with Northwest flow, the positive anomaly of the water vapor flux transported from Western Pacific to Huaxi region strengthened, caused precipitation increase in east Huaxi region. During 1980 to 1999, when the IOD in autumn was positive phase, the atmospheric circulation presented a “W” shape at 500 hPa, the positive anomaly of the water vapor flux transported from Bay of Bengal to Huaxi region strengthened, caused precipitation ascend in west Huaxi region. In summary, the Indian Ocean changed from cold phase to warm phase since the 1970s, caused the instability of the inter-annual relationship between the IOD and the autumn rainfall in Huaxi region.  相似文献   

17.
正While China’s Air Pollution Prevention and Control Action Plan on particulate matter since 2013 has reduced sulfate significantly, aerosol ammonium nitrate remains high in East China. As the high nitrate abundances are strongly linked with ammonia, reducing ammonia emissions is becoming increasingly important to improve the air quality of China. Although satellite data provide evidence of substantial increases in atmospheric ammonia concentrations over major agricultural regions, long-term surface observation of ammonia concentrations are sparse. In addition, there is still no consensus on  相似文献   

18.
基于最新的GTAP8 (Global Trade Analysis Project)数据库,使用投入产出法,分析了2004年到2007年全球贸易变化下南北集团贸易隐含碳变化及对全球碳排放的影响。结果显示,随着发展中国家进出口规模扩张,全球贸易隐含碳流向的重心逐渐向发展中国家转移。2004年到2007年,发达国家高端设备制造业和服务业出口以及发展中国家资源、能源密集型行业及中低端制造业出口的趋势加强,该过程的生产转移导致全球碳排放增长4.15亿t,占研究时段全球贸易隐含碳增量的63%。未来发展中国家的出口隐含碳比重还将进一步提高。贸易变化带来的南北集团隐含碳流动变化对全球应对气候变化行动的影响日益突出,发达国家对此负有重要责任。  相似文献   

19.
Using the International Comprehensive Ocean-Atmosphere Data Set(ICOADS) and ERA-Interim data, spatial distributions of air-sea temperature difference(ASTD) in the South China Sea(SCS) for the past 35 years are compared,and variations of spatial and temporal distributions of ASTD in this region are addressed using empirical orthogonal function decomposition and wavelet analysis methods. The results indicate that both ICOADS and ERA-Interim data can reflect actual distribution characteristics of ASTD in the SCS, but values of ASTD from the ERA-Interim data are smaller than those of the ICOADS data in the same region. In addition, the ASTD characteristics from the ERA-Interim data are not obvious inshore. A seesaw-type, north-south distribution of ASTD is dominant in the SCS; i.e., a positive peak in the south is associated with a negative peak in the north in November, and a negative peak in the south is accompanied by a positive peak in the north during April and May. Interannual ASTD variations in summer or autumn are decreasing. There is a seesaw-type distribution of ASTD between Beibu Bay and most of the SCS in summer, and the center of large values is in the Nansha Islands area in autumn. The ASTD in the SCS has a strong quasi-3a oscillation period in all seasons, and a quasi-11 a period in winter and spring. The ASTD is positively correlated with the Nio3.4 index in summer and autumn but negatively correlated in spring and winter.  相似文献   

20.
正AIMS AND SCOPE Atmospheric and Oceanic Science Letters (AOSL) publishes short research letters on all disciplines of the atmosphere sciences and physical oceanography. Contributions from all over the world are welcome.SUBMISSIONAll submitted  相似文献   

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