Network Flow and Ford-Fulkerson Algorithm

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[Blank] meteorology deals with the study of physical processes of the atmosphere.

Physical

[Blank] is the average weather conditions taken over a long time.

Climate

[Blank] meteorology deals with large scale meteorological conditions.

Macro

The word meteorology is derived from two Greek words: Meteor and ______.

<p>logus</p> Signup and view all the answers

[Blank] deals with the atmospheric phenomena which are in motion.

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[Blank] observation are taken on the ground or in the atmosphere to get a synoptic view of the world's weather.

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[Blank] meteorology is the study of the climate of a place or region on the basis of long periods of time.

<p>Climatology</p> Signup and view all the answers

Meteorology means events occurring above the earth ______.

<p>surface</p> Signup and view all the answers

[Blank] is the atmospheric conditions at a given time and place.

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[Blank] meteorology deals with the application of meteorology to human activities.

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[Blank] meteorology deals with the study of atmospheric processes by means of experiments in the laboratory.

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The study of small scale meteorological conditions is called ______ meteorology.

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Issues such as climate change and global warming are receiving increasing ______.

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[Blank] is defined as the science which deals with the study of water bodies and water cycle.

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[Blank] is the study of the interractions between atmospheric processes and all living organisms.

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The equations for dynamic meteorology are solved to derive a final ______.

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Weather changes from hour to hour and from day to ______.

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The radiations absorption and scattering in the earth-atmosphere system are studied processes of ______ meteorology.

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Meteorologists use weather information and adopt the findings of ______ research to suit a specific application.

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[Blank] normals are derived from a data base that extends for decades.

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Flashcards

Weather

Atmospheric conditions at a given time and place with reference to temperature, pressure, moisture, wind speed and direction, cloud and sky conditions.

Climate

Average weather conditions taken over a long time (20, 30 or 50yrs). It also includes the extremes and mean weather conditions.

Meteorology

The word meteorology is derived from two Greek words: Meteor and logus. Meteor means events occurring above the earth surface and logus means to study.

Climatology

Climatology is the study of the climate of a place or region on the basis of weather records accumulated over long periods of time.

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Dynamic Meteorology

Deals with the atmospheric phenomena which are in motion, describing atmospheric processes through mathematical equations (numerical models).

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Physical Meteorology

Deals with the study of physical processes of the atmosphere. Study the physical processes of the atmosphere such as solar radiation, its absorption and scattering in the earth-atmosphere system.

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Experimental Meteorology

It is a branch of meteorology which deals with the study of atmospheric processes by means of experiments in the laboratory as well as in the field e.g. cloud formation experiment in the laboratory and rain making experiments in the field.

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Synoptic Meteorology

Deals with the study of synoptic observations plotted on weather charts for forecasting. Studies the movement of pressure areas, air masses, fronts and weather systems.

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Micrometeorology

Deals with the study of small scale meteorological conditions close to the Earth's surface, involving refined measurements near the ground.

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Macrometeorology

Deals with the study of large scale meteorological conditions. Relates to large geographical regions (continents or the entire globe).

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Hydrology

Branch of meteorology dealing with water bodies and the water cycle within the earth atmosphere system.

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Biometeorology

An interdisciplinary science dealing with meteorology and climatology to biological systems, including the effect of atmospheric conditions on living organisms.

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Study Notes

Network Flow

  • A flow network is a directed graph G = (V, E) featuring a source node s ∈ V, a sink node t ∈ V, and a capacity c(u, v) ≥ 0 for each edge (u, v) ∈ E.
  • A flow is a function f: V × V → ℝ that satisfies the capacity constraint, skew symmetry, and flow conservation.
    • The capacity constraint is expressed such that for all u, v ∈ V, f(u, v) ≤ c(u, v)
    • Skew symmetry implies that for all u, v ∈ V, f(u, v) = -f(v, u)
    • Flow conservation is such that for all u ∈ V \ {s, t}, ∑v ∈ V f(u, v) = 0
  • The value of a flow f is given by |f| = ∑v ∈ V f(s, v)
  • The maximum-flow problem aims to find a flow of maximum value in a given flow network G.

Ford-Fulkerson Algorithm

  • This algorithm is used to solve the maximum-flow problem in a network
  • It initializes the flow f(u, v) = 0 for all u, v ∈ V.
  • The algorithm iterates as long as there exists an augmenting path p in G.
    • It finds a path p from s to t in Gf, where Gf is the "residual network".
    • It calculates cf(u, v) = c(u, v) - f(u, v)
    • It sets cf(p) = min{cf(u, v) : (u, v) is in p}
    • For each edge (u, v) in p: f(u, v) = f(u, v) + cf(p) and f(v, u) = f(v, u) - cf(p)
  • Returns f.

Definitions for Ford-Fulkerson

  • Residual capacity of an edge (u, v) is calculated as cf(u, v) = c(u, v) - f(u, v).
    • It represents the additional flow that can be pushed from u to v.
  • The residual network of G induced by f is Gf = (V, Ef), where Ef = {(u, v) ∈ V × V : cf(u, v) > 0}.
    • These edges can admit more flow.
  • An augmenting path is a simple path from s to t in Gf.

Max-Flow Min-Cut Theorem

  • A cut (S, T) of a flow network G = (V, E) is a partition of V into S and T = V \ S such that s ∈ S and t ∈ T.
  • The capacity of a cut (S, T) is defined as c(S, T) = ∑u ∈ S ∑v ∈ T c(u, v).
  • The flow across a cut (S, T) is defined as f(S, T) = ∑u ∈ S ∑v ∈ T f(u, v).
  • Max-Flow Min-Cut Theorem: For a flow f in a flow network G = (V, E), the following conditions are equivalent:
    • f is a maximum flow in G.
    • The residual network Gf contains no augmenting paths.
    • |f| = c(S, T) for some cut (S, T) of G.

Eigenvalues and Eigenvectors Definitions

  • For an n × n matrix A, a scalar λ is considered an eigenvalue if there exists a non-zero vector v such that Av = λv.
  • If λ is an eigenvalue of A, then v is an eigenvector of A corresponding to λ.
  • For an n × n matrix A, a scalar λ is an eigenvalue if and only if det(A - λI) = 0.

Finding Eigenvalues and Eigenvectors

  • For an n × n matrix A:
    • Solve the characteristic equation det(A - λI) = 0 for λ.
    • For each eigenvalue λ, solve the homogeneous system (A - λI)v = 0 for the eigenvectors v.

Example 1: Find Eigenvalues and Eigenvectors

  • Solve for matrix A = [1 3; 4 2]
  • The eigenvalues of A are λ1 = 5 and λ2 = -2.
  • The eigenvector corresponding to λ1 = 5 is v1 = [3; 4].
  • The eigenvector corresponding to λ2 = -2 is v2 = [1; -1].

Example 2: Find Eigenvalues and Eigenvectors

  • Solve for matrix A = [2 -1; 5 -2]
  • The eigenvalues are λ = ±i.
  • For λ1 = i, the corresponding eigenvector is v1 = [1; 2 - i].
  • For λ2 = -i, the corresponding eigenvector is v2 = [1; 2 + i].

Example 3: Find Eigenvalues and Eigenvectors

  • Solve for A = [1 2 1; 0 1 0; 0 1 3]
  • The eigenvalues are λ1 = 1 and λ2 = 3.
  • The eigenvector corresponding to λ1 = 1 is v1 = [1; 0; 0].
  • The eigenvector corresponding to λ2 = 3 is v2 = [1; 0; 2].

Theorem 1 Relating to Eigenvalues

  • For an n × n matrix A, the following are equivalent:
    • λ is an eigenvalue of A.
    • (A - λI)v = 0 has nontrivial solutions.
    • The linear system (A - λI)v = 0 has infinitely many solutions.
    • A - λI is singular.
    • det(A - λI) = 0.

Theorem 2 Relating to Eigenvalues

  • If A is a triangular matrix, its eigenvalues are the entries on the main diagonal.

Geometric Vectors (Chapter 1, Linear Algebra and Analytic Geometry I)

  • A geometric vector is an oriented line segment.
  • The vector from point A to point B is denoted as $\overrightarrow{AB}$, where A is the origin, and B is the endpoint.
  • The length of the segment is the norm, denoted as $|\overrightarrow{AB}|$.
  • The direction of $\overrightarrow{AB}$ is that of the line (AB), and the sense is from A to B.
  • Two vectors are equal if they share the same norm, direction, and sense.
  • A vector with a norm of 1 is a unit or normalized vector.
  • The vector whose origin and endpoint coincide is the zero vector, $\vec{0}$, with a norm of zero and no direction or sense.
  • The opposite of a vector $\overrightarrow{AB}$ is $\overrightarrow{BA}$, denoted as $-\overrightarrow{AB}$.

Vector Operations

  • The sum of two vectors $\vec{u}$ and $\vec{v}$ is found by placing the origin of $\vec{v}$ at the endpoint of $\vec{u}$.
    • $\vec{u} + \vec{v}$ connects the origin of $\vec{u}$ to the endpoint of $\vec{v}$.
  • (Parallelogram Rule): If $\vec{u}$ and $\vec{v}$ share an origin, $\vec{u} + \vec{v}$ is the diagonal of the parallelogram formed by $\vec{u}$ and $\vec{v}$.

Vector Addition Properties

  • Commutativity: $\vec{u} + \vec{v} = \vec{v} + \vec{u}$
  • Associativity: $(\vec{u} + \vec{v}) + \vec{w} = \vec{u} + (\vec{v} + \vec{w})$
  • Identity Element: $\vec{u} + \vec{0} = \vec{u}$
  • Inverse Element: $\vec{u} + (-\vec{u}) = \vec{0}$

Scalar Multiplication

  • Multiplying a vector $\vec{u}$ by a scalar $\lambda \in \mathbb{R}$ results in a vector $\lambda\vec{u}$ with the same direction as $\vec{u}$.
    • The norm is $|\lambda||\vec{u}|$, and the sense is the same as $\vec{u}$ if $\lambda > 0$, or opposite if $\lambda < 0$.
    • If $\lambda = 0$ or $\vec{u} = \vec{0}$, then $\lambda\vec{u} = \vec{0}$.

Scalar Multiplication Properties

  • Associativity: $\lambda(\mu\vec{u}) = (\lambda\mu)\vec{u}$
  • Distributivity over scalar addition: $(\lambda + \mu)\vec{u} = \lambda\vec{u} + \mu\vec{u}$
  • Distributivity over vector addition: $\lambda(\vec{u} + \vec{v}) = \lambda\vec{u} + \lambda\vec{v}$
  • Identity element: $1\vec{u} = \vec{u}$

Linear Combination of Vectors

  • A linear combination of vectors $\vec{u}_1, \vec{u}_2,..., \vec{u}_n$ is a vector like this: $\lambda_1\vec{u}_1 + \lambda_2\vec{u}_2 +... + \lambda_n\vec{u}_n$, where $\lambda_1, \lambda_2,..., \lambda_n \in \mathbb{R}$.

Analytical Vector Representation

  • In a Cartesian plane $(O, \vec{i}, \vec{j})$, every vector $\vec{u}$ can be uniquely expressed as $\vec{u} = u_1\vec{i} + u_2\vec{j}$, where $u_1$ and $u_2$ are components of $\vec{u}$ in the base $(\vec{i}, \vec{j})$.
    • $\vec{u} = (u_1, u_2)$
  • In a Cartesian space $(O, \vec{i}, \vec{j}, \vec{k})$, every vector $\vec{u}$ can be uniquely expressed as $\vec{u} = u_1\vec{i} + u_2\vec{j} + u_3\vec{k}$, where $u_1$, $u_2$, and $u_3$ are components of $\vec{u}$ in the base $(\vec{i}, \vec{j}, \vec{k})$.
    • $\vec{u} = (u_1, u_2, u_3)$

Vector Component Operations

  • Given vectors $\vec{u} = (u_1, u_2, u_3)$, $\vec{v} = (v_1, v_2, v_3)$, and scalar $\lambda \in \mathbb{R}$:
    • $\vec{u} + \vec{v} = (u_1 + v_1, u_2 + v_2, u_3 + v_3)$
    • $\lambda\vec{u} = (\lambda u_1, \lambda u_2, \lambda u_3)$
    • $\vec{0} = (0, 0, 0)$
    • $-\vec{u} = (-u_1, -u_2, -u_3)$

Vector Norm

  • The norm of $\vec{u} = (u_1, u_2, u_3)$ is $|\vec{u}| = \sqrt{u_1^2 + u_2^2 + u_3^2}$.
    • In the plane, $|\vec{u}| = \sqrt{u_1^2 + u_2^2}$.

Distance Between Two Points

  • The distance between points $A(x_1, y_1, z_1)$ and $B(x_2, y_2, z_2)$ is $d(A, B) = |\overrightarrow{AB}| = \sqrt{(x_2 - x_1)^2 + (y_2 - y_1)^2 + (z_2 - z_1)^2}$.
    • In the plane, $d(A, B) = \sqrt{(x_2 - x_1)^2 + (y_2 - y_1)^2}$.

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