Source of low frequency modulation of ENSO amplitude in a CGCM     

Byung-Kwon Moon  Sang-Wook Yeh  Boris Dewitte  Jong-Ghap Jhun  In-Sik Kang 《Climate Dynamics》2007,29(1):101-111

We study the relationship between changes in equatorial stratification and low frequency El Niño/Southern Oscillation (ENSO) amplitude modulation in a coupled general circulation model (CGCM) that uses an anomaly coupling strategy to prevent climate drifts in the mean state. The stratification is intensified at upper levels in the western and central equatorial Pacific during periods of high ENSO amplitude. Furthermore, changes in equatorial stratification are connected with subsurface temperature anomalies originating from the central south tropical Pacific. The correlation analysis of ocean temperature anomalies against an index for the ENSO modulation supports the hypothesis of the existence of an oceanic “tunnel” that connects the south tropical Pacific to the equatorial wave guide. Further analysis of the wind stress projection coefficient onto the oceanic baroclinic modes suggests that the low frequency modulation of ENSO amplitude is associated with a significant contribution of higher-order modes in the western and central equatorial Pacific. In the light of these results, we suggest that, in the CGCM, change in the baroclinic mode energy distribution associated with low frequency ENSO amplitude modulation have its source in the central south tropical Pacific.  相似文献   

Interaction Between A Fast Plasmoid and the Solar Wind     

Wang  S.  Wang  X.Y.  Wu  C.S.  Li  Y.  Chao  J.K.  Yeh  T. 《Solar physics》2001,202(2):385-393

In this note a kinetic interaction process between a fast plasmoid ejected by the Sun, which represents another form of CME, and the background solar wind in the corona is discussed. We consider a system which consists of the plasmoid ions moving faster than the solar wind. We are interested in the time evolution of the ion distribution functions due to wave–particle interactions. Simulation results show that both perpendicular and parallel temperatures of the solar wind ions increase when the relative velocity between the plasmoid and the solar wind is sufficiently greater than the Alfvén velocity of the plasmoid ions. We suggest that this process is significant for the heating and acceleration of the solar wind in the low-heliographic latitude regions near the Sun.  相似文献   

Topological structure of coronal-interplanetary magnetic field     

Tyan Yeh 《Solar physics》1978,56(2):439-447

The topological structure of the coronal-interplanetary magnetic field is determined by the arrangement of the neutral lines at the coronal base. It is characterized by nested separatrices, which are interfaces between closed and open field lines or between oppositely directed open field lines, in the coronal-interplanetary space. In the neighborhoods of these separatrices there are important electric currents. These currents form the basis for the sheet-current model.The National Center for Atmospheric Research is sponsored by the National Science Foundation.  相似文献   

Three-dimensional V_P and V_S structural models associated with the active subduction and collision tectonics in the Taiwan region     

Kwang-Hee Kim  Jer-Ming Chiu  Jose Pujol  Kou-Cheng Chen  Bor-Shouh Huang  Yih-Hsiung Yeh  Peng Shen 《Geophysical Journal International》2005,162(1):204-220

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Influence of river channel geometry in stream flow modelling and guidelines for field investigation          下载免费PDF全文

Hongbo Zhang  Fan Zhang  Xiaonan Shi  Chen Zeng  Dong‐Sin Shih  Gour‐Tsyh Yeh  Daniel R. Joswiak 《水文研究》2014,28(4):2630-2638

Fully physics‐based, process‐level, distributed fluid flow and reactive transport hydrological models are rarely used in practice until recent years. These models are useful tools to help understand the fundamental physical, chemical, and biological processes that take place in nature. In this study, sensitivity analyses based on a mountain area river basin modelling study are performed to investigate the effect of river channel geometric characteristics on downstream water flow. Numerical experiments show that reduction in the river channel geometric measurement interval may not significantly affect the downstream water stage simulation as long as measurement accuracy at special nodes is guaranteed. The special upstream nodes include but are not limited to 1) nodes located close to the observation station, 2) nodes near the borders of different land covers with considerable riverbed roughness changes, 3) nodes at entering points of tributaries causing discharge jump and 4) nodes with a narrow cross‐section width that may control the flow conditions. This information provides guidelines for field investigation to efficiently obtain necessary geometric data for physics‐based hydrological modelling. It is especially useful in alpine areas such as the Tibetan Plateau where field investigation capability is limited under severe topography and climate condition. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   

Erratum to: Analysis of pumping test data for determining unconfined-aquifer parameters: Composite analysis or not?     

Hund-Der Yeh  Yen-Chen Huang 《Hydrogeology Journal》2010,18(8):1983-1983

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Reactive transport codes for subsurface environmental simulation     

C. I. Steefel  C. A. J. Appelo  B. Arora  D. Jacques  T. Kalbacher  O. Kolditz  V. Lagneau  P. C. Lichtner  K. U. Mayer  J. C. L. Meeussen  S. Molins  D. Moulton  H. Shao  J. Šimůnek  N. Spycher  S. B. Yabusaki  G. T. Yeh 《Computational Geosciences》2015,19(3):445-478

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Review: Optimization methods for groundwater modeling and management     

William W-G Yeh 《Hydrogeology Journal》2015,23(6):1051-1065

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An analysis on movement patterns between zones using smart card data in subway networks     

Kwanho Kim  Kyuhyup Oh  Yeong Kyu Lee  SungHo Kim 《International journal of geographical information science》2014,28(9):1781-1801

Identifying zones and movement patterns of people is crucial to understanding adjacent regions and the relationship in urban areas. Most previous studies addressed zones or movement patterns separately without analysing simultaneously the two issues. In this article, we propose an integrated approach to discover directly both zones and movement patterns among the zones, referred to as movement patterns between zones (MZPs), from historical boarding behaviours of passengers in subway networks by using an agglomerative clustering method. In addition, evaluation measures of MZPs are suggested in terms of coverage and accuracy. The effectiveness of the proposed approach is finally demonstrated through a real-world data set obtained from smart cards on a subway network in Seoul, Korea.  相似文献   

Combined effect of El Niño-Southern Oscillation and Pacific Decadal Oscillation on the East Asian winter monsoon   总被引：1，自引：0，他引：1  

Ji-Won Kim  Sang-Wook Yeh  Eun-Chul Chang 《Climate Dynamics》2014,42(3-4):957-971

Using long-term observational data and numerical model experiments, the combined effect of the El Niño-Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) on the variability of the East Asian winter monsoon is examined. In the observations, it is found that when the ENSO and PDO are in-phase combinations (i.e., El Niño/positive PDO phase and La Niña/negative PDO phase), a negative relationship between ENSO and East Asian winter monsoon is significantly intensified. In other words, when El Niño (La Niña) occurs with positive (negative) PDO phase, anomalous warm (cold) temperatures are dominant over the East Asian winter continent. On the other hand, there are no significant temperature anomalies when the ENSO and PDO are out-of-phase combinations (i.e., El Niño/negative PDO phase and La Niña/positive PDO phase). Further analyses indicate that the anticyclone over the western North Pacific including the East Asian marginal seas plays an essential role in modulating the intensity of the East Asian winter monsoon under the changes of ENSO–PDO phase relationship. Long-lasting high pressure and warm sea surface temperature anomalies during the late fall/winter and following spring over the western North Pacific, which appear as the El Niño occurs with positive PDO phase, can lead to a weakened East Asian winter monsoon by transporting warm and wet conditions into the East Asian continent through the southerly wind anomalies along the western flank of the anomalous high pressure, and vice versa as the La Niña occurs with negative PDO phase. In contrast, the anomalous high pressure over the western North Pacific does not show a prominent change under the out-of-phase combinations of ENSO and PDO. Numerical model experiments confirm the observational results, accompanying dominant warm temperature anomalies over East Asia via strong anticyclonic circulation anomalies near the Philippine Sea as the El Niño occurs with positive PDO phase, whereas such warming is weakened as the El Niño occurs with negative PDO phase. This result supports the argument that the changes in the East Asian winter monsoon intensity with ENSO are largely affected by the strength of the anticyclone over the western North Pacific, which significantly changes according to the ENSO–PDO phase relationship.  相似文献