In addition, the game somehow gets more beautiful with Frozen Wilds with
great snow effects and beautiful lighting (and draw distance).
Not exact matches
The environments by and large look
great, with the constantly falling
snow being a brilliant added
effect.
I embellished my version and added extra details, but it gave a
great introduction to using the painting knife to create fantastic
snow covered
effects.
I've touched on lake -
effect snows, the classic pattern in the Upper Midwest and western New York State in which frigid winds blowing over relatively warm
Great Lakes waters generate persistent cloud bands and lots of
snow.
Re 9 wili — I know of a paper suggesting, as I recall, that enhanced «backradiation» (downward radiation reaching the surface emitted by the air / clouds) contributed more to Arctic amplification specifically in the cold part of the year (just to be clear, backradiation should generally increase with any warming (aside from greenhouse feedbacks) and more so with a warming due to an increase in the greenhouse
effect (including feedbacks like water vapor and, if positive, clouds, though regional changes in water vapor and clouds can go against the global trend); otherwise it was always my understanding that the albedo feedback was key (while sea ice decreases so far have been more a summer phenomenon (when it would be warmer to begin with), the heat capacity of the sea prevents much temperature response, but there is a
greater build up of heat from the albedo feedback, and this is released in the cold part of the year when ice forms later or would have formed or would have been thicker; the seasonal
effect of reduced winter
snow cover decreasing at those latitudes which still recieve sunlight in the winter would not be so delayed).
The warmer those lake temperatures, the more moisture in the air, and the
greater potential for lake
effect snows.
Lake
effect snow near the
great lakes results from substantial warming of the lakes in the summer months and heat carryover causing evaporation into the early part of the following winter.
Is it not also therefore true that the polar areas of least water vapor, where a
greater temperature increase from doubling of Co-2 would have the most
effect, has the least W / sq - m percentage of both incoming S - W and outgoing L - W radiation due to the incident angle of incoming Sun light, the high reflectivity of the
snow and ice, and the greatly reduced outgoing L - W radiation due to this?
Is it not also therefore true that the polar areas of least water vapor, where a
greater temperature increase from doubling of Co-2 would have the most
effect, has the least percentage of both incoming S - W and outgoing L - W radiation due to the incident angle of incoming Sun light, the high reflectivity of the
snow and ice, and the greatly reduced outgoing L - W radiation due to this?
In this data activity, students interpret raw data on
snow cover and explore the climatic impact of the «lake
effect» - a significant factor determining snowfall amount in the
Great Lakes drainage basin is the surface temperature of the lakes... (View More) Step - by - step instructions for use of the MY NASA DATA Live Access Server (LAS) guide students through selecting a data set, importing the data into a spreadsheet, creating graphs, and analyzing data plots.
Models disagree on
snow water equivalent changes on a regional basis, especially in transitional regions where competing
effects occur due to
greater snowfall and warming temperatures.»
While it is true that warmer temperatures can produce heavier
snow — as anyone who lives within range of lake -
effect snow, which mostly falls before the
Great Lakes freeze over or become too cold to generate the condensation responsible for heavy
snow, can attest — we have been seeing both heavier
snow and colder temperatures, both in the United States and in Europe, and not merely this winter, but for a number of winters running.