• News & Views
    Adv. Atmos. Sci.
    Calculating grid-cell aerosol direct shortwave radiative forcing
    It is an effective approach to calculate grid-cell ADRF at large scales by using the SBDART model im...
    Arctic sea ice loss and the Eurasian winter cooling trend: Is there a link?
    One particular topic of interest has been the recent cooling of winter temperatures over the Eurasia...
    Scientist emphasizes importance of multi-level thinking
    The paper touches on a range of deep questions within and outside the atmospheric sciences. They in...
    Current Issue
      07 August 2017 , Volume 34 Issue 9   
    Determining the Spectrum of the Nonlinear Local Lyapunov Exponents in a Multidimensional Chaotic System
    Ruiqiang DING,Jianping LI,Baosheng LI
    2017 , 34 (9 ): 1027 -1034.   DOI: 10.1007/s00376-017-7011-8
    Abstract ( 59 )   HTML   PDF (1005 KB) ( 60 )

    For an n-dimensional chaotic system, we extend the definition of the nonlinear local Lyapunov exponent (NLLE) from one- to n-dimensional spectra, and present a method for computing the NLLE spectrum. The method is tested on three chaotic systems with different complexity. The results indicate that the NLLE spectrum realistically characterizes the growth rates of initial error vectors along different directions from the linear to nonlinear phases of error growth. This represents an improvement over the traditional Lyapunov exponent spectrum, which only characterizes the error growth rates during the linear phase of error growth. In addition, because the NLLE spectrum can effectively separate the slowly and rapidly growing perturbations, it is shown to be more suitable for estimating the predictability of chaotic systems, as compared to the traditional Lyapunov exponent spectrum.

    Figures and Tables | References | Related Articles | Metrics
    Evaluating Common Land Model Energy Fluxes Using FLUXNET Data
    Xiangxiang ZHANG,Yongjiu DAI,Hongzhi CUI,Robert E. DICKINSON,Siguang ZHU,Nan WEI,Binyan YAN,Hua YUAN,Wei SHANGGUAN,Lili WANG,Wenting FU
    2017 , 34 (9 ): 1035 -1046.   DOI: 10.1007/s00376-017-6251-y
    Abstract ( 20 )   HTML   PDF (612 KB) ( 43 )

    Given the crucial role of land surface processes in global and regional climates, there is a pressing need to test and verify the performance of land surface models via comparisons to observations. In this study, the eddy covariance measurements from 20 FLUXNET sites spanning more than 100 site-years were utilized to evaluate the performance of the Common Land Model (CoLM) over different vegetation types in various climate zones. A decomposition method was employed to separate both the observed and simulated energy fluxes, i.e., the sensible heat flux, latent heat flux, net radiation, and ground heat flux, at three timescales ranging from stepwise (30 min) to monthly. A comparison between the simulations and observations indicated that CoLM produced satisfactory simulations of all four energy fluxes, although the different indexes did not exhibit consistent results among the different fluxes. A strong agreement between the simulations and observations was found for the seasonal cycles at the 20 sites, whereas CoLM underestimated the latent heat flux at the sites with distinct dry and wet seasons, which might be associated with its weakness in simulating soil water during the dry season. CoLM cannot explicitly simulate the midday depression of leaf gas exchange, which may explain why CoLM also has a maximum diurnal bias at noon in the summer. Of the eight selected vegetation types analyzed, CoLM performs best for evergreen broadleaf forests and worst for croplands and wetlands.

    Figures and Tables | References | Related Articles | Metrics
    Simulated Sensitivity of the Tropical Cyclone Eyewall Replacement Cycle to the Ambient Temperature Profile
    Xulin MA,Jie HE,Xuyang GE
    2017 , 34 (9 ): 1047 -1056.   DOI: 10.1007/s00376-017-6302-4
    Abstract ( 19 )   HTML   PDF (1194 KB) ( 45 )

    In this study, the impacts of the environmental temperature profile on the tropical cyclone eyewall replacement cycle are examined using idealized numerical simulations. It is found that the environmental thermal condition can greatly affect the formation and structure of a secondary eyewall and the intensity change during the eyewall replacement cycle. Simulation with a warmer thermal profile produces a larger moat and a prolonged eyewall replacement cycle. It is revealed that the enhanced static stability greatly suppresses convection, and thus causes slow secondary eyewall formation. The possible processes influencing the decay of inner eyewall convection are investigated. It is revealed that the demise of the inner eyewall is related to a choking effect associated with outer eyewall convection, the radial distribution of moist entropy fluxes within the moat region, the enhanced static stability in the inner-core region, and the interaction between the inner and outer eyewalls due to the barotropic instability. This study motivates further research into how environmental conditions influence tropical cyclone dynamics and thermodynamics.

    Figures and Tables | References | Related Articles | Metrics
    Observation-based Estimation of Aerosol-induced Reduction of Planetary Boundary Layer Height
    Jun ZOU,Jianning SUN,Aijun DING,Minghuai WANG,Weidong GUO,Congbin FU
    2017 , 34 (9 ): 1057 -1068.   DOI: 10.1007/s00376-016-6259-8
    Abstract ( 11 )   HTML   PDF (1465 KB) ( 33 )

    Radiative aerosols are known to influence the surface energy budget and hence the evolution of the planetary boundary layer. In this study, we develop a method to estimate the aerosol-induced reduction in the planetary boundary layer height (PBLH) based on two years of ground-based measurements at a site, the Station for Observing Regional Processes of the Earth System (SORPES), at Nanjing University, China, and radiosonde data from the meteorological station of Nanjing. The observations show that increased aerosol loads lead to a mean decrease of 67.1 W m-2 for downward shortwave radiation (DSR) and a mean increase of 19.2 W m-2 for downward longwave radiation (DLR), as well as a mean decrease of 9.6 W m-2 for the surface sensible heat flux (SHF) in the daytime. The relative variations of DSR, DLR and SHF are shown as a function of the increment of column mass concentration of particulate matter (PM2.5). High aerosol loading can significantly increase the atmospheric stability in the planetary boundary layer during both daytime and nighttime. Based on the statistical relationship between SHF and PM2.5 column mass concentrations, the SHF under clean atmospheric conditions (same as the background days) is derived. In this case, the derived SHF, together with observed SHF, are then used to estimate changes in the PBLH related to aerosols. Our results suggest that the PBLH decreases more rapidly with increasing aerosol loading at high aerosol loading. When the daytime mean column mass concentration of PM2.5 reaches 200 mg m-2, the decrease in the PBLH at 1600 LST (local standard time) is about 450 m.

    Figures and Tables | References | Related Articles | Metrics
    Analysis of Spatial Autocorrelation Patterns of Heavy and Super-Heavy Rainfall in Iran
    Iman ROUSTA,Mehdi DOOSTKAMIAN,Esmaeil HAGHIGHI,Hamid Reza GHAFARIAN MALAMIRI,Parvane YARAHMADI
    2017 , 34 (9 ): 1069 -1081.   DOI: 10.1007/s00376-017-6227-y
    Abstract ( 35 )   HTML   PDF (27529 KB) ( 45 )

    Rainfall is a highly variable climatic element, and rainfall-related changes occur in spatial and temporal dimensions within a regional climate. The purpose of this study is to investigate the spatial autocorrelation changes of Iran's heavy and super-heavy rainfall over the past 40 years. For this purpose, the daily rainfall data of 664 meteorological stations between 1971 and 2011 are used. To analyze the changes in rainfall within a decade, geostatistical techniques like spatial autocorrelation analysis of hot spots, based on the Getis-Ord Gi statistic, are employed. Furthermore, programming features in MATLAB, Surfer, and GIS are used. The results indicate that the Caspian coast, the northwest and west of the western foothills of the Zagros Mountains of Iran, the inner regions of Iran, and southern parts of Southeast and Northeast Iran, have the highest likelihood of heavy and super-heavy rainfall. The spatial pattern of heavy rainfall shows that, despite its oscillation in different periods, the maximum positive spatial autocorrelation pattern of heavy rainfall includes areas of the west, northwest and west coast of the Caspian Sea. On the other hand, a negative spatial autocorrelation pattern of heavy rainfall is observed in central Iran and parts of the east, particularly in Zabul. Finally, it is found that patterns of super-heavy rainfall are similar to those of heavy rainfall.

    Figures and Tables | References | Related Articles | Metrics
  • Impact Factor: 1.483
  • ISSN 0256-1530
  • CN 11-1925/04

  • Back Issues
  • Early Online Release
  • Most Read Articles
  • Email Alert
  • FUN Publishing with AAS
  • ISSN 0256-1530
  • CN 11-1925/04
  • 京ICP备14024088号
  • Tel:86-10-82995054,86-10-82995055
  • Fax:86-10-82995053
  • Zip/Postal Code:100029
  • E-mail: aas@mail.iap.ac.cn
  • Copyright © 2015 ADVANCES IN ATMOSPHERIC SCIENCES