#aos — Public Fediverse posts

🛫🌤🛬 CBR > OOL

#AoS  

🛫🌤🛬 CBR > OOL

#AoS  

🛫🌤🛬 CBR > OOL

#AoS  

🛫🌤🛬 CBR > OOL

#AoS  

🛫🌤🛬 CBR > OOL

#AoS  

#TheCleavermaws are #PirateOrruks wholly obsessed with magic.

Narg Tideshouta is a Warchanter, laden with a collection of the juiciest artefacts, often picked because they resonate with his war-chants and horrible sea-shanties.

https://warbosskurgan.blogspot.com/2026/06/the-ironfang-fleet-warchanter-for.html

#AgeOfSigmar #Warhammer #WarhammerCommunity #WarHamFam #Nerdlings #AoS #Warcry #Ironjawz

The #RumourEngine for 9th June 2026

Perfectly normal sword. Totally safe.

https://warbosskurgan.blogspot.com/p/rumour-engines.html#2026-06-09

#Warhammer #WarhammerCommunity #WarHamFam #Nerdlings #AgeOfSigmar #AoS #WH40K #Chaos #Daemons

Last weekend I ran Unfallen - a narrative Warcry event, at #UKGE

10 players were asked to choose their path through the blighted wilds of Thyria: as either Contaminators seeding creeping corruption, or Remediators sworn to burn out the rot and restore balance.

https://warbosskurgan.blogspot.com/2026/06/unfallen-ukge-2026-warcry-narrative.html

#UKGamesExpo #UKGE2026
#Warcry #NarrativePlay #Warhammer #AgeOfSigmar #AoS #WarHamFam #WarhammerCommunity

The #RumourEngine for 2nd June 2026

Lizardy... talons?... claws?

Foot. Lizardy foot.

https://warbosskurgan.blogspot.com/p/rumour-engines.html#2026-06-02

#Warhammer #WarhammerCommunity #WarHamFam #Nerdlings #AgeOfSigmar #AoS #Dragon

Basics of Numerical Weather Prediction (NWP):

1. THE HORIZONTAL MOMENTUM EQUATION:
\[
\frac{d\mathbf{V}}{dt} + f\hat{k} \times \mathbf{V} = -\nabla \phi + \frac{\sigma}{p_s} \frac{\partial \phi}{\partial \sigma} \nabla p_s + \mathbf{F}
\]

2. THE CONTINUITY EQUATION:
\[
\frac{\partial p_s}{\partial t} + \nabla \cdot (p_s \mathbf{V}) + \frac{\partial}{\partial \sigma}(p_s \dot{\sigma}) = 0
\]

3. THE THERMODYNAMIC ENERGY EQUATION:
\[
\frac{1}{R} \frac{d}{dt} \left[ \sigma \frac{\partial \phi}{\partial \sigma} \right] + \frac{RT}{C_p p} \left[ p_s \dot{\sigma} + \sigma\dot{p_s} \right] = -Q
\]

4. HYDROSTATIC EQUATION:
\[
\frac{\partial \phi}{\partial \sigma} = -\frac{RT_v}{\sigma}
\]

5. SURFACE PRESSURE TENDENCY EQUATION:
\[\displaystyle
\frac{\partial p_s}{\partial t} = -\int_{0}^{1} \nabla\cdot (p_s \mathbf{V}) \, d\sigma
\]

6. MOISTURE EQUATION:
\[\displaystyle
\frac{\partial}{\partial t} (p_s q) + \nabla\cdot (p_s q \mathbf{V}) + \frac{\partial}{\partial \sigma} (p_s q \dot{\sigma}) = p_s S
\]

The six primary unknowns are: \(\mathbf{V}\) (horizontal wind velocity), \(p_s\) (surface pressure), \(T\) (temperature), \(q\) (specific humidity or moisture), \(\phi\) (geopotential), and \(\dot{\sigma}\) (sigma velocity or vertical velocity in \(\sigma\)-coordinates).

#NWP #Weather #NumericalWeatherPrediction #Meteorology #Climate #ClimateScience #Earth #EarthScience #ClimateChange #ClimateSciences #Science #WeatherPrediction #Humidity #Moisture #Pressure #Velocity #SurfacePressure #HydrostaticEquation #WeatherPrediction #Ocean #Atmosphere #AOS #ClimateDynamics #WeatherDynamics #Geopotential #SigmaVelocity #VerticalVelocity #MoistureEquation #Thermodynamics #Dynamics #NavierStokes