哈雷彗星的彗发光谱     

谢光中  茶光伟  卢汝为  李晓渝  郝鹏九  鲍梦贤  张云 《中国天文和天体物理学报》1989,(2)

用云南天文台一米望远镜卡焦摄谱仪(f=175mm相机),在哈雷彗星的日心距分别为1.11AU和0.83AU时,作了两次彗发光谱观测,得到了典型的彗发光谱。本文绘出了各带系清晰的分子发射光谱图及认证结果。此外,本文还给出了彗发CN的(0—1)带(λ4216)和C_3的蓝紫发射(λ4052)及C_2的(2—0)带(λ4365)的强度比CN/C_3和CN/C_2,其值分别为CN/C_3=1.03,CN/C_2=1.00。最后,我们还将结果与其他作者在这次回归中所得到的结果进行了比较。  相似文献   

Evaluation of climatological tropical cyclone activity over the western North Pacific in the CORDEX-East Asia multi-RCM simulations     

Chun-Sil Jin  Dong-Hyun Cha  Dong-Kyou Lee  Myoung-Seok Suh  Song-You Hong  Hyun-Suk Kang  Chang-Hoi Ho 《Climate Dynamics》2016,46(3-4):765-778

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Runoff and sediment yield modeling using SWAT model: case of Wadi Hatab basin,central Tunisia   总被引：1，自引：0，他引：1  

Narjes Chaâbane Ben Salah  Habib Abida 《Arabian Journal of Geosciences》2016,9(11):579

This study presents an application of the model Soil and Water Assessment Tool (SWAT) to simulate daily and monthly water flow and sediment fluxes in the Wadi Hatab watershed (2200 km²) located in central Tunisia. The study basin is characterized by a significant climatic contrast, abrupt topography, and soil fragility, resulting thereby in flash floods and important water erosion rates. This alarming situation requires urgent interventions in order to preserve water and soil resources, implying the need for a decision tool for proper integrated management of the watershed. The model was calibrated and validated based on a comparison of simulated and observed flow rates at the basin outlet (hydrometric station Khanguet Zazia), during the periods 1987–1988 and 1989–1990, respectively. The comparison was based not only on visual inspection of the agreement between observed and simulated time series, but also on statistical parameters. Indeed, for the daily time step application, the Nash—Sutcliffe efficiency (NSE) values were 0.52 and 0.61, and the coefficient of determination (R²) was 0.54 and 0.61 for calibration and validation, respectively. As for the monthly time-step application, the obtained NSE values were 0.67 and 0.89 while R² values were 0.83 and 0.87 for calibration and validation, respectively. This clearly shows the reasonably good agreement between simulated and observed flow rates. In terms of erosion, the model gave sediment yield values ??of 1.15 and 5.37 t/ha/year during the periods of calibration and validation, respectively.  相似文献   

Change in future tropical cyclone activity over the western North Pacific under global warming scenario     

Ki-Seon Choi  Yu-Mi Cha 《Natural Hazards》2012,64(2):1125-1140

Differences in atmospheric and oceanic environments which affect the tropical cyclone (TC) activity between the late twenty-first century (2071?C2100, A1B) and the late twentieth century (1971?C2000, 20C3M) are analyzed using multi-model ensemble from 15 general circulation models. Six factors (vertical wind shear, 700?hPa relative humidity, 850?hPa relative vorticity, outgoing longwave radiation, precipitation, and sea surface temperature) related to TC genesis predicts that more TCs in the future will occur than in the present. The result of maximum potential intensity analysis shows the frequency of occurrence and influence of stronger TCs will increase over the western North Pacific in the future. Anomalous northerly in the mid-latitudes of East Asia due to the strengthening of west-high and east-low pressure system pattern in the future plays an important role in blocking TC from moving toward mid-latitudes of East Asia. The multiple linear regression model (MLRM) developed using six predictors (independent variables) analyzed from NCEP-NCAR reanalysis data predicts that total TC genesis frequency during July to October (JASO), which predicted using data of 20C3M, will have more (2?C3) TCs than in the present.  相似文献   

Cluster analysis of tropical cyclone tracks around Korea and its climatological properties     

Ki-Seon Choi  Yu-Mi Cha  Tae-Ryong Kim 《Natural Hazards》2012,64(1):1-18

After the fuzzy clustering method (FCM) that analyzes the tracks of the tropical cyclones (TCs) struck the Korean peninsula (hereafter, K-TC) for a 60-year period (1951?C2010), it is found that both frequency and intensity of K-TC have been increased in recent years. In the order of the cluster number, both K-TC track pattern and its full-track pattern tended to shift southward. That is, while the passage frequency of TC in mainland China and the Manchurian regions decreased, it instead over the sea. Due to this decrease in the topographic effect on TC before reaching Korea, TC intensity around Korea became stronger. The vertical wind shear well reflected a TC intensity around Korea, which became weaker in mid-latitudes of East Asia. On the other hand, the peak month of K-TC frequency lags in the order of the cluster number. The two clusters that most TCs pass through the Korean Peninsula showed a stronger intensity and higher frequency before the 1970s. Meanwhile, another two clusters that most TCs pass through the Straits of Korea or the western region of the Japanese Islands showed those characteristics from the 1980s onward. Consequently, the changes in TC track, recurvature, frequency, and intensity around Korea were related to the southward shift of the western North Pacific high in the order of the cluster number.  相似文献   

Protostellar collapse induced by compression – II. Rotation and fragmentation     

P. Hennebelle  A. P. Whitworth  S.-H. Cha  S. P. Goodwin 《Monthly notices of the Royal Astronomical Society》2004,348(2):687-701

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The evolutionary sequence of Fermi blazars     

Yongjuan Cha  Haojing Zhang  Xiong Zhang  Dingrong Xiong  Bijun Li  Xia Dong  Jin Li 《Astrophysics and Space Science》2014,349(2):895-908

Using γ-ray data (α _γ , F _γ ) detected by Fermi Large Area Telescope (LAT) and black hole mass which has been compiled from literatures for 116 Fermi blazars, we calculated intrinsic γ-ray luminosity, intrinsic bolometric luminosity, intrinsic Eddington ratio and studied the relationships between all above parameters and redshift, between α _γ and L _γ . Furthermore, we obtained the histograms of key parameters. Our results are the following: (1) The main reason for the evolutionary sequence of three subclasses (HBLs, LBLs, FSRQs) may be Eddington ratio rather than black hole mass; (2) FSRQs occupy in the earlier, high-luminosity, high Eddington ratio, violent phase of the galactic evolution sequence, while BL Lac objects occur in the low luminosity, low Eddington ratio, late phase of the galactic evolution sequence; (3) These results imply that the evolutionary track of Fermi blazars is FSRQs ? LBLs ? HBLs.  相似文献   

Fermi gamma-ray and multi-wave band emission from TeV active galactic nuclei     

Dingrong Xiong  Haojing Zhang  Xiong Zhang  Yonggang Zheng  Wenguang Liu  Lisheng Mao  Bangrong Huang  Ting Kang  Yongjuan Cha  Fei Guo 《Astrophysics and Space Science》2013,343(1):345-360

Using γ-ray data detected by Fermi Large Area Telescope (LAT) and multi-wave band data for 40 TeV active galactic nuclei (AGNs), we have studied the correlations between flux densities (F _R, F _IR, F _O, F _X and F _γ ) in the radio, infrared, optical, X-ray and γ-ray wave bands. Our results are the following: (1) For TeV HSP BL Lacertae objects (THBLs), there are strong correlations between F _γ and F _R and between F _γ and F _IR in all states (average/high/low); (2) The TeV radio galaxies (TRGs) deviate from the area occupied by THBLs; (3) The TeV flat-spectrum radio quasars (TFSRQs) have much stronger γ-ray emission than THBLs; (4) For THBLs, there are weak correlations between F _γ and F _X in all states as well as between F _γ and F _O in both average and high states, and a strong correlation between F _γ and F _O in the low state; (5) For THBLs, there are strong correlations between F _O and F _R in both low and average states as well as between F _O and F _IR in all states and between F _IR and F _R in all states, but no strong correlations among other bands are found. From these results, we suggest that for THBLs, the synchrotron self-Compton radiation (SSC) is the main mechanism of high energy γ-ray emission and the inverse Compton scattering of circum-nuclear dust is likely to be a important complementary mechanism. Compared with THBLs, TRGs and TFSRQs may have a different origin of high energy γ-ray.  相似文献   

Interdecadal changes in TC activities that affect Korea     

Ki-Seon Choi  Yu-Mi Cha  Sung-Dae Kang  Hae-Dong Kim 《Theoretical and Applied Climatology》2014,116(3-4):491-500

The present study elucidated the fact that remarkable interdecadal variation exists in the time series of the tropical cyclone (TC) frequency that affects Korea during June–October. These variations were identified through statistical change-point analysis, and the results showed that significant variation existed in 1983 and 2004. Therefore, data in 2005 and thereafter were excluded and differences in TC activities during the period after 1983 (1984–2004) and a period before 1983 (1968–1983), as well as differences in large-scale environments were analyzed. During the period of 1984–2004, TCs mainly occurred in the northwest quadrant of the subtropical western North Pacific (SWNP). The TCs move from the east sea of Philippines, pass the East China Sea, recurved, and moved to Korea and Japan. During the period of 1968–1983, TCs occurred in the southeast quadrant of the SWNP and showed a characteristic westward movement from the southeast of Philippines toward the southern coast of China and the Indochina Peninsula. Therefore, the intensity of TCs during the former period, which were supplied with greater heat and water vapor from the sea, were stronger, while TCs during the latter period quickly dissipated after landing in the southern coast of China and the Indochina Peninsula due to the effects of topography. Thus, the lifetimes of the TCs were short and their intensities were weak. The cause of these differences in TC activities between the two periods was identified through differences in stream flows between the 850 hPa level and the 500 hPa level. At the 850 hPa level, anomalous cyclonic (anticyclonic) circulations are reinforced in most waters north (south) to 10° N, and thus, more (fewer) TCs occur in the northwest (southeast) quadrant of the SWNP during the period of 1984–2004 (1968–2003). At the 500 hPa level, since the center of anomalous cyclonic circulation is located in the southeastern region of China southeast to the east sea of the Philippines, anomalous southerlies from the east sea of Philippines to Korea and Japan are predominant. Due to the anomalous steering flows of these anomalous southerlies, the TCs during the period of 1984–2004 show the aforementioned paths. On the other hand, anomalous northerlies or northeasterlies are reinforced in regions in the west of the center of these anomalous cyclonic circulations, and thus, these anomalous steering flows serve the role of preventing TCs from moving toward the southern coast of China the Indochina Peninsula during the period of 1984–2004. During the period of 1984–2004, vertical wind shears and sea surface temperatures are high and low, respectively, in most waters of the SWNP. Therefore, more TCs occur and are reinforced during this period.  相似文献   

Limited change in dune mobility in response to a large decrease in wind power in semi-arid northern China since the 1970s   总被引：2，自引：0，他引：2  

Joseph A. Mason  James B. Swinehart  Huayu Lu  Xiaodong Miao  Phueng Cha  Yali Zhou 《Geomorphology》2008,102(3-4):351-363

The climatic controls on dune mobility, especially the relative importance of wind strength, remain incompletely understood. This is a key research problem in semi-arid northern China, both for interpreting past dune activity as evidence of paleoclimate and for predicting future environmental change. Potential eolian sand transport, which is approximately proportional to wind power above the threshold for sand entrainment, has decreased across much of northern China since the 1970s. Over the same period, effective moisture (ratio of precipitation to potential evapotranspiration) has not changed significantly. This “natural experiment” provides insight on the relative importance of wind power as a control on dune mobility in three dunefields of northern China (Mu Us, Otindag, and Horqin), although poorly understood and potentially large effects of human land use complicate interpretation. Dune forms in these three regions are consistent with sand transport vectors inferred from weather station data, suggesting that wind directions have remained stable and the stations adequately represent winds that shaped the dunes. The predicted effect of weaker winds since the 1970s would be dune stabilization, with lower sand transport rates allowing vegetation cover to expand. Large portions of all three dunefields remained stabilized by vegetation in the 1970s despite high wind power. Since the 1970s, trends in remotely sensed vegetation greenness and change in mobile dune area inferred from sequential Landsat images do indicate widespread dune stabilization in the eastern Mu Us region. On the other hand, expansion of active dunes took place farther west in the Mu Us dunefield and especially in the central Otindag dunefield, with little overall change in two parts of the Horqin dunes. Better ground truth is needed to validate the remote sensing analyses, but results presented here place limits on the relative importance of wind strength as a control on dune mobility in the study areas. High wind power alone does not completely destabilize these dunes. A large decrease in wind power either has little short-term effect on the dunes, or more likely its effect is sufficiently small that it is obscured by human impacts on dune stability in many parts of the study areas.  相似文献