commit 5d26e04a67bdd953811492d633a688f07f74decf
parent 4de846e13d01be826d446f210125407fc06133c2
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date: Mon, 28 Jun 2021 08:31:08 +0200
011-james.txt: fix references and style
Diffstat:
1 file changed, 10 insertions(+), 10 deletions(-)
diff --git a/pages/011-james.txt b/pages/011-james.txt
@@ -1,18 +1,18 @@
Considerable areas of the polar oceans are covered by sea ice,
-formed by frozen sea water. The extent and thickness of the ice
-pack influences local and regional ecology and climate. The ice
+formed by frozen sea water. The extent and thickness of the ice
+pack influences local and regional ecology and climate. The ice
thickness is particularly important for the ice-cover survival
-during warm summers. Wind and ocean currents compress and shear the
-sea ice, and can break and stack ice into ridges. Current sea ice
-models assume that the ice becomes increasingly rigid as ridges of
-ice rubble grow. Modeling sea ice as bonded particles, we show that
-ice becomes significantly weaker right after the onset of ridge
-building. We introduce a mathematical framework that allows these
+during warm summers. Wind and ocean currents compress and shear
+the sea ice, and can break and stack ice into ridges. Current sea
+ice models assume that the ice becomes increasingly rigid as ridges
+of ice rubble grow. Modeling sea ice as bonded particles, we show
+that ice becomes significantly weaker right after the onset of ridge
+building. We introduce a mathematical framework that allows these
physical processes to be included in large-scale models.
Today a [1]new paper of mine is published in the AGU-group journal
-[1]Journal of Advances in Modeling Earth Systems, and it is written
-with co-authors Olga Sergienko and Alistair Adcroft at Princeton
+[2]Journal of Advances in Modeling Earth Systems, and it is written
+with co-authors [3]Olga Sergienko and [4]Alistair Adcroft at Princeton
University (New Jersey, USA). I use my program [5]Granular.jl for
the simulations.
