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Mostly MWTO with azimuth thrusters are
equippedwithaccelerationnozzles.Nozzlesprevent
propellersfromdamageandincreasetheirefficiency.
Where acceleration nozzles are applicable, open
water propeller force should be multiplied by
respectiveaccelerationcoefficient.
Power resources, which are represented by
Energysubsystem,shouldbesimulatedaccordingto
MWTO classification
society approved Power
ManagementPlan.
Step 4. MWTO motion control mathematical
description. During this step, hierarchical
performance of Computation and Information
subsystems are described. Computation subsystem
mathematical description involves development of
station keeping and low speed maneuvering
algorithms on MWTO mathematical model basis.
Informationsubsystemprovidesdata fromdifferent
sources
for these algorithms. This data include
MWTO position, kinematics and dynamics,
disturbance and reaction forces in different
coordinate systems, power reserve, thruster
allocation and set point, etc. Forces distribution
algorithm computes necessary forces for each
availablethrustertoperformDPoperations.
Stage 2. EF system dynamics mathematical
description is carried out
on the basis of
meteorological data and DP locally confined area
analysis. At this stage, depending on the used
method and accuracy requirements, the following
shouldbedetermined:EFcharacteristics,characterof
hydrological features (Froude number, tide heights,
etc.). The EF conditions could be also defined as a
one minute
mean maximum wind velocity, a most‐
probable significant wave height, and a most‐
probablewavemodalperiod.
Thelibraryofwaterareasiscreatedonthisstage.
SystematicEFwaterareadataincludethefollowing:
generalweatherconditionsinlocallyconfinedareaof
DPoperations,characteristicsofwindspeedandits
direction, characteristics of sea state (wave heights,
swelldirection),characteristicsofcurrentspeedand
itsdirection(peculiaritiesofchanges).
Step1.Nonlinearwindmodel.Windisdefinedas
the movement of air relative to the surface of the
Earth. Mathematical models of wind forces and
momentsimproveperformance androbustness
ofthe
system in extreme conditions.The nature of the
nonlinear component depends on the water area of
MWTO operation. The appropriate spectral
characteristicsmayalsobeused.
Step 2. Nonlinear wave model. The process of
wave generation due to wind starts with small
wavelets appearing on the water area surface.
This
increasesthe dragforce, whichinturn allowsshort
wavesto grow.Short wavescontinue to grow until
they finally break and their energy is dissipated. A
developingsea,orstorm,startswithhighfrequencies
creating a spectrum with a peak at a relative high
frequency.Astorm,which
haslastedforalongtime,
creates a fully developed sea. After the wind has
stopped, a low frequency decaying sea or swell is
formed. These long waves form a wave spectrum
with a low peak frequency. If the swell from one
storminteractswiththewavesfromanotherstorm,a
wave spectrum with two peak frequencies may be
observed. In addition, tidal waves will generate a
peakat alowfrequency. Hence,the resultingwave
spectrummightbequitecomplicatedinwaterareas,
wheretheweatherchangesrapidly.
Step 3. Nonrotational current model. Current is
definedashorizontalmotionof
watersystemswitha
constantaveragespeed.Verticalmovementofwater
particlesfromonelayertoanotherisnotconsidered.
Stage 3. MWTO‐EF interaction. Step 1. MWTO‐
wind interaction. Assumption of wind flow
homogeneityandquasi‐stationarypropertiesplay s a
major role in the mathematical description of the
MWTOreaction
towinddisturbance.Calculationof
wind forces and moments acting on MWTO results
fromrelativewindspeedandangleisdone.
Step 2. MWTO‐wave interaction. The interaction
of MWTO hull with waves is a complex physical
process.ThemathematicaldescriptionoftheMWTO
reaction on the wave disturbance requires
consideration on regular and irregular waves.In
the first case, the model will have deterministic
nature,andinthesecond‐astochasticnature.Wave‐
inducedforcesandmomentonMWTOarecalculated
using force transfer function. Wave height is a
governing factor of this function. Research of the
stochastic model is
more complicated and time
consuming,butresultsmoreaccuratelydescribethe
reactiontothewavedisturbance.
Step3.MWTO‐currentinteraction.The natureof
the MWTO reaction depends on the current speed
and direction. All hull protractions hydrodynamic
effectiscalculatedonthisstepaswell.Consideration
of current speed
changes, caused by hydrological
featuresofthewaterarea,improvestheaccuracyof
results.
Inordertoreceiveparametersofthestatevector
to evaluate MWTO safety of DP operations, which
undergononlinearEFdisturbances,itisnecessaryto
make description of the MWTO subsystems
interaction, which are coordinated to solve
the
followingtasks:
Decompositionofcomplexsystemsandtasksinto
moresimple(typicalorstandard).
Relationship determination between selected
componentsinthelogicalgorithmsform.
Distributed processing by Computation
subsystem of various primary data from
Information subsystem. During this process,
navigation regarding MWTO dynamic
positioning in locally
confined space are formed
andrepresentedtoDPO.
Distributed secondary processing of aggregation
orgroupdata, whichtogetherreflectMWTOstate
vector characteristics and EF disturbance main
vector characteristics (course over ground,
heading, speed, direction and force of
disturbances).
Determination of threat directions that form
extremesituationconcerningDP
safety.
Parameters identification (for components of
Controlled thrusters and Energy subsystems),
which are required for safe and effective DP
processrealizationinlocallyconfinedarea.
Realization of identified parameters by DP
processcontrollaws.