Explaining Intraday Pattern of Trading Volume from the Order Flow Data

Order Flow and the Monetary Model of Exc

Order Flow and the Monetary Model of Exchange Rates: Evidence from a Novel Data Set

✍ MENZIE D. CHINN; MICHAEL J. MOORE 📂 Article 📅 2011 🏛 John Wiley and Sons 🌐 English ⚖ 580 KB

On the definition of the flow width for

On the definition of the flow width for calculating specific catchment area patterns from gridded elevation data

✍ Giovanni Battista Chirico; Andrew W. Western; Rodger B. Grayson; Günter Blöschl 📂 Article 📅 2005 🏛 John Wiley and Sons 🌐 English ⚖ 212 KB

Specific catchment area (SCA) patterns are commonly computed on grids using flow direction algorithms that treat the flow as coming from a point source at the pixel centre. These algorithms are all ambiguous in the definition of the flow width to be associated with a pixel when computing the SCA. Di

Relict Shorelines and Ice Flow Patterns

Relict Shorelines and Ice Flow Patterns of the Northern Puget Lowland From Lidar Data and Digital Terrain Modelling

✍ Dori J. Kovanen; Olav Slaymaker 📂 Article 📅 2004 🏛 John Wiley and Sons 🌐 English ⚖ 910 KB

The global network of plate boundaries c

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid-plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.

✍ L.-E. Ricou 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 197 KB

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin