Sinking Alloyances

Alloyances = Alloys + Alliances

sedimentation.mp4
"Sedimentation from a buoyant freshwater plume"
10.1002/2016JC012053

Halite (salt)
14 cm x 12 cm x 11 cm
150 x 138 pixels
NaCl

Shadow_Graphs.wav
65.869.456 bytes
44100 Hz / 6:13"

Common cordgrass (Spartina)
Geometry Triangles 46.9k
Vertices 41.3k

a time of ups

a time of downs

along flows of trade

and hence of debt

a monoculture of remoteness

long term capture

agile trade with the non living

in subsurface kingdom dysphoria

measuring a time

in tense symmetry

a time of downs

along flows of trade

a monoculture of remoteness

long term capture

agile trade with the non living

in subsurface kingdom dysphoria

measuring a time

in tense symmetry

a time of ups

along flows of trade

and hence of debt

a monoculture of remoteness

long term capture

agile trade with the non living

in subsurface kingdom dysphoria

measuring a time

in tense symmetry

a time of ups

a time of downs

Great Bay

East River

Lake Borgne

Pamlico Sound

Amapa mangroves

Guianan mangroves

Manabi Mangroves

Unterelbe

Sundarbans Mangrove

Fraser River

Amazon River

Thames Estuary

New York-New Jersey Harbor

Dawei River Estuary

Albemarle Sound

Long Island Sound

Narragansett Bay

Belizean Coast Mangroves

Rio de la Plata

Waeru River Estuary

Western Scheldt

Bahia Mangroves

Spencer Gulf

Golden Horn

The basis for area-based carbon stock accounting is an equation to estimate the changes in carbon stock within and between land cover classes, with each characterized as a fraction (ai) of the total area (A) (the stratum weighting) and each with a time-dependent carbon stock density Cᵢ,𝑡(the stratum mean). ∆C−>𝑡->𝑡+₁ = A𝑡{ⁿ∑ᵢ=₁(aᵢ,𝑡 (Cᵢ,𝑡+₁ − Cᵢ )+(aᵢ,𝑡+₁ − aᵢ )Cᵢ,𝑡)}. ∆C = annual change in carbon stocks in the landscape in Mg yr-1 or t yr-1. Carbon stock density consists of the aboveground and belowground biomass, aboveground necromass and soil organic matter. The total annual change of carbon stock at the landscape level is the sum of the area of each transition of land uses multiplied by the total changes in C stock for each transition per unit area, divided by the time period.