我国中东部一次大范围霾天气的分析   总被引：27，自引：4，他引：23  

饶晓琴  李峰  周宁芳  杨克明 《气象》2008,34(6):89-96

利用空气污染资料、常规气象观测资料和NCEP再分析资料,对2007年2月5日我国中东部大范围霾天气进行了综合分析.结果表明:前倾槽结构和逆温层结为霾的形成提供了有利条件;800hPa以下层垂直速度、涡度和散度的绝对值较小.是霾维持的动力因子.大气混合层高度的变化对霾的生消有很好指示作用,霾天混合层高度北高南低分布,致使南方比北方更易出现严重霾天气.此外,要素对比结果表明,霾的相对湿度比雾低,温度露点差比雾大,逆温强度比雾弱,大气混合层高度比雾高,这些可为霾的预报提供参考依据.  相似文献   

四川省邻水县土壤锌地球化学特征及玉米水稻籽实锌含量预测          下载免费PDF全文

马旭东  余涛  杨忠芳  张虎生  武芝亮  王珏  李明辉  雷风华 《中国地质》2022,49(1):324-335

[研究目的]锌(Zn)是一种人体所必需的微量元素.利用区域地球化学调查数据,准确预测农作物中Zn含量,从而开展富Zn农产品开发规划仍存在较大难度.[研究方法]本文选择四川省邻水县为研究区,依据土地质量地球化学调查所获得的表层土壤、农作物及根系土中地球化学指标数据,系统研究了土壤与农作物中Zn含量和空间分布特征,分析了玉...  相似文献   

Assessment of Slope Stability for Deep Pits in Sedimentary Strata     

Brett A. Poulsen  Deepak P. Adhikary  Rao Balusu 《Geotechnical and Geological Engineering》2017,35(2):631-643

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Evidence for Neoarchean basement for the Deccan Volcanic flows around Koyna-Warna region,western India: Zircon U-Pb age and Hf-isotopic results     

Y. J. Bhaskar Rao  B. Sreenivas  T. Vijaya Kumar  Namrata Khadke  A. Kesava Krishna  E. V. S. S. K. Babu 《Journal of the Geological Society of India》2017,90(6):752-760

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Impacts of mesoscale eddies in the South China Sea on biogeochemical cycles   总被引：1，自引：1，他引：0  

Mingxian Guo  Fei Chai  Peng Xiu  Shiyu Li  Shivanesh Rao 《Ocean Dynamics》2015,65(9-10):1335-1352

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Effect of Salinity and Currents on Sea Level Variation Along the Indian Coast: A Numerical Study     

A. D. Rao  S. V. Babu  S. K. Dube 《Marine Geodesy》2013,36(1-2):145-158

The process of upwelling/sinking and associated sea level variations are seen as a response of coastal ocean to pure wind stress forcing. Further,precipitation and monsoonal floods, apart from the marine meteorological parameters, are expected to influence the sea level fluctuations along the coast. This study comprises determining the sea level from the various parameters together with the pure wind stress forcing, which is compared with the observed cycle. However, it is found that there is considerable difference between the computations and observations. This suggests that the sea level is dependent not just on the local forcing alone, but also on the induced background circulation as well. For example, the sea level changes along the east coast of India, particularly the northern region, are more sensitive to freshwater discharge from various rivers joining the Bay of Bengal. This is due to more frequently occurring pre- and postmonsoon cyclonic storms and the associated surges in the Bay of Bengal as compared to the Arabian Sea. Hence the salinity effects are particularly important in the coastal waters off the east coast of India during monsoon months (June-September). For the west coast of India, however, it is expected that the large-scale coastal circulation may play a role in determining sea level changes in addition to other forcings. The salinity effects are negligible along the west coast in the absence of any major river systems that join the Arabian Sea. The local advection currents caused by the offshore directed freshwater discharge from various estuaries joining the coastal bay also seemed to influence the sea level. In order to elucidate the essential dynamics involved and to study the effect of the remote forcing, a three-dimensional baroclinic, nonlinear numerical model is used with appropriate open boundary conditions. The local effect of the current has been incorporated in the west coast model by means of opening a channel at Cochin through which the rainwater is carried away to the model ocean. The low saline plume, cascading from north along the east cost of India, has been incorporated in the east coast model through a proper forcing applied at the northern boundary of the model. With the inclusion of these remote forcings in the models, the disagreement between the simulations and the observations is minimized.  相似文献   

Behavior of a helical anchor under vertical repetitive loading     

S. Narasimha Rao  Y. V. S. N. Prasad 《Marine Georesources & Geotechnology》2013,31(3-4):203-228

Abstract

In the field of ocean engineering, anchors are used for several purposes. This article studies the behavior of a helical anchor embedded in soft marine clay under vertical repetitive loading. Helical anchors are simple steel shafts to which one or more helical plates are attached at regular intervals. The tests are conducted on a model helical anchor installed in a soft marine clay bed prepared in a test tank. Repetitive loading is applied using a pneumatic loading arrangement. Different cyclic load ratios and time periods are adopted. In each test, after the application of repetitive loading, poststatic‐pullout tests are conducted to observe the effect of repetitive loading on anchor behavior. From the test results, it is found that, up to a cyclic load ratio of 55%, there is no reduction in capacity. Instead, there seems to be a marginal increase in capacity and reduction in displacement. The reasons for this behavior are explained in terms of induced changes in strength and deformation behavior of marine clay under repetitive load. However, at higher cyclic load ratios, there seems to be reduction in pullout capacity of the anchor, and the reason for this is explained in terms of strain criteria. From this investigation, it can be concluded that the deep anchor is more suitable to a marine environment than a shallow anchor.  相似文献   

CORONA satellite photographs — A new (Old) tool for earth scientists     

K. Nageswara Rao 《Journal of the Geological Society of India》2009,73(3):425-429

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Uplifted crust in parts of western India   总被引：1，自引：0，他引：1  

H. C. Tewari  G. Surya Prakasa Rao  B. Rajendra Prasad 《Journal of the Geological Society of India》2009,73(4):479-488

During northward movement of the Indian sub-continent, after its breakup from the Gondwanaland in the Late Cretaceous, the western part of India traversed over the Reunion plume. The Saurashtra peninsula and the Cambay Basin are two important geological regions in this part. Two and half dimensional density models, based on the crustal seismic structure, were generated to establish a relationship between these two regions. These models indicate that the crust is 32–33 km thick in the eastern Saurashtra and the northern part of the Cambay Basin. The shallower crust is in a triangular region formed by the extension of the western limb of the Proterozoic Aravalli trend in Saurashtra, its eastern limb and the Narmada fault in the south. Compared to 36–37 km thick crust to the west and 38–40 km to the east of this region the crust in the above triangular region is uplifted by 4 to 6 km. This uplift took place either after the deposition of Mesozoic sediments or was concomitant with the rise of Reunion plume prior to the extrusion of the Deccan volcanics as the region was close to the axis of the plume.  相似文献   

Track prediction of very severe cyclone ‘Nargis’ using high resolution weather research forecasting (WRF) model   总被引：1，自引：0，他引：1  

D. R. Pattanaik  Y. V. Rama Rao 《Journal of Earth System Science》2009,118(4):309-329

The recent very severe cyclonic storm (VSCS) ‘Nargis’ over the Bay of Bengal caused widespread destruction over Myanmar after hitting the coast on 2 May 2008. The real time forecasting of the VSCS ‘Nargis’ was a very difficult task as it did not follow the normal westerly/northwesterly track. In the present study, a detailed diagnostic analysis of the system ‘Nargis’ is carried out initially to investigate the features associated with this unusual movement and subsequently the real time forecast of VSCS ‘Nargis’ using high resolution advanced version weather research forecasting (WRF) model is presented. The advanced research WRF model was run for 72 h at 27 km and 20 km resolutions with 28, 29, 30 April and 1 May as the initial conditions. The diagnostic study indicates that the recurvature of the system ‘Nargis’ was mainly associated with:

•	upper level southerly/southwesterly steering wind at 200 hPa level associated with anticyclonic circulation over southeastern sector of the centre of the system
•	higher SST (29°C or more) with higher positive anomalies over the region to the northeast of the cyclone centre, and
•	large negative 24 h pressure changes and large vorticity maximum to the east of the system.

The real time track forecast using the WRF model run at 27 km and 20 km resolution based on the initial conditions of 28 April (when the system was only 550 km away from the Indian coast) indicated that the system had a northeasterly forecast track and was not expected to cross the Indian coast. Similarly, based on 29 April initial condition the system showed east/east-northeasterly movement towards the Myanmar coast. The east/east-northeasterly movement of the ‘Nargis’ was persisting in the forecast based on 30 April and 1 May initial conditions with respective landfall errors of 85 km and 50 km with 27 km resolution, which reduces to 30 km and 40 km respectively with 20 km resolution, however, with a landfall time delay of about 10 h. Improvement of mean forecast errors at different forecast hours is noticed in WRF model run at higher resolution compared to that run at lower resolution. Thus, it is very clear that the advanced version WRF model had captured movement of the system reasonably well almost 3 days in advance. Consistence with the diagnostic analysis the WRF model forecast also indicates southerly/southwesterly strong steering wind at 200 hPa level and maximum pressure fall to the east of the system.  相似文献