Search Results

You are looking at 101 - 110 of 183 items for :

  • Journal of Hydrometeorology x
  • All content x
Clear All
Isidora Jankov, Jian-Wen Bao, Paul J. Neiman, Paul J. Schultz, Huiling Yuan, and Allen B. White

>2.0.CO;2 Marwitz, J. , 1983 : The kinematics of orographic airflow during Sierra storms. J. Atmos. Sci. , 40 , 1218 – 1227 . 10.1175/1520-0469(1983)040<1218:TKOOAD>2.0.CO;2 Mattioli, V. , Westwater E. R. , Cimini D. , Liljegren J. S. , Lesht B. M. , Gutman S. I. , and Schmidlin F. J. , 2007 : Analysis of radiosonde and ground-based remotely sensed PWV data from the 2004 North Slope of Alaska Arctic Winter Radiometric Experiment. J. Atmos. Oceanic Technol. , 24 , 415

Full access
John Kochendorfer, Michael E. Earle, Daniel Hodyss, Audrey Reverdin, Yves-Alain Roulet, Rodica Nitu, Roy Rasmussen, Scott Landolt, Samuel Buisán, and Timo Laine

-s intervals. With the exception of the HSA, all gauges performed an internal intensity correction to compensate for kinematic effects (precipitation losses between successive tips of the collection mechanism) at higher intensities. The reference precipitation measurements were recorded using the double-fence automated reference (DFAR) configuration at each site. Each DFAR consisted of a weighing precipitation gauge (either an OTT Pluvio2, from OTT Hydromet, Kempten, Germany, or a 3-wire T-200B3

Open access
Jonathan J. Gourley, Yang Hong, Zachary L. Flamig, Jiahu Wang, Humberto Vergara, and Emmanouil N. Anagnostou

runoff is kinematically routed downstream based on cell connectivity, slope, and flow direction derived from a digital elevation model. Two parameters describe the channel routing component. A power-law equation employing a coefficient and exponent is used to describe the relation between discharge and cross-sectional area. These parameters are found empirically using measurements of cross-sectional area and discharge at the USGS stream-gauging site circled in Fig. 1 . Forcing to HL-RDHM includes

Full access
Ryan J. MacDonald, James M. Byrne, and Stefan W. Kienzle

air (2.25 × 10 −5 m 2 s −1 ). The Nusselt number N Nu and Sherwood number N sh are where the Reynolds number N re = (2 r Vr/ V ); Vr is the terminal ventilation velocity, where horizontal particle components are assumed equal to the horizontal wind speed ( Schmidt 1982 ; Déry and Taylor 1996 ), and V is the kinematic viscosity of air (1.53 × 10 −5 m 2 s −1 ; Déry and Yau 1999 ). 4) Snowmelt The snowmelt routine was adopted from Quick and Pipes (1977) . For snowmelt to

Full access
Ming-Hsu Li, Ming-Jen Yang, Ruitang Soong, and Hsiao-Ling Huang

. , 239 , 19 – 32 . Jasper, K. , Gurtz J. , and Lang H. , 2002 : Advanced flood forecasting in Alpine watersheds by coupling meteorological observations and forecasts with a distributed hydrological model. J. Hydrol. , 267 , 40 – 52 . 10.1016/S0022-1694(02)00138-5 Lee, W-C. , Jou B. J-D. , Chang P-L. , and Deng S-M. , 1999 : Tropical cyclone kinematical structure retrieved from single-Doppler radar observations. Part I: Interpolation of Doppler velocity patterns and the GBVTD

Full access
Tomoko Nitta, Kei Yoshimura, and Ayako Abe-Ouchi

predictions of the temperature and amount of water in the canopy, soil, and snow. The freezing and melting of soil water are also considered. As shown in the gray box in the upper-left part of Fig. 2 , water inflow to the soil surface goes to infiltration or to surface runoff directly to rivers. The kinematic wave equation is used for river routing ( Ngo-Duc et al. 2007 ). Fig . 1. Land cover of the potential vegetation tiles used in this study: 1) continental ice, 2) broadleaf evergreen forest, 3

Full access
Gerhard Smiatek and Harald Kunstmann

Green and Ampt (1911) . The estimation of the saturation time is after Peschke (1987) , and it uses translation-retention and kinematic wave approaches in the lateral runoff aggregation. In the application with daily input data, the potential evapotranspiration has been calculated following the approach of Hamon ( Hamon 1961 ). In the setup of the present experiment, land cover data from the Coordination of Information on the Environment (CORINE) database at 100-m spatial resolution were included

Full access
Jeffrey P. Walker, Garry R. Willgoose, and Jetse D. Kalma

model of basin hydrology. Hydrol. Sci. Bull , 24 , 43 – 69 . 10.1080/02626667909491834 Boughton, W. C. , 1983 : A simple model for estimating the water yield of ungauged catchments. Civ. Eng. Trans , CE25 , 83 – 88 . Cabral, M. C. , Garrote L. , Bras R. L. , and Entekhabi D. , 1992 : A kinematic model of infiltration and runoff generation in layered and sloped soils. Adv. Water Resour , 15 , 311 – 324 . 10.1016/0309-1708(92)90017-V Capehart, W. J. , and Carlson T. N

Full access
James V. Rudolph and Katja Friedrich

. , 2008 : The VGAM package. R News, Vol. 8, No. 2, R Foundation for Statistical Computing, Hamilton, ON, Canada, 28–39 . Yee, T. W. , and Hastie T. J. , 2003 : Reduced-rank vector generalized linear models . Stat. Modell. , 3 , 15 – 41 . Yuter, S. E. , and Houze R. A. Jr. , 1995 : Three-dimensional kinematic and microphysical evolution of Florida cumulonimbus. Part II: Frequency distributions of vertical velocity, reflectivity, and differential reflectivity . Mon. Wea. Rev. , 123

Full access
Amin K. Dezfuli, Benjamin F. Zaitchik, Hamada S. Badr, Jason Evans, and Christa D. Peters-Lidard

the recent Syrian drought . Proc. Natl. Acad. Sci. USA , 112 , 3241 – 3246 , doi: 10.1073/pnas.1421533112 . 10.1073/pnas.1421533112 Kingsmill , D. E. , P. J. Neiman , B. J. Moore , M. Hughes , S. E. Yuter , and F. M. Ralph , 2013 : Kinematic and thermodynamic structures of Sierra barrier jets and overrunning atmospheric rivers during a landfalling winter storm in Northern California . Mon. Wea. Rev. , 141 , 2015 – 2036 , doi: 10.1175/MWR-D-12-00277.1 . 10.1175/MWR-D-12

Full access