The novel takes Bill Harsker from the fields of France to other postings in the post war world of 1918. It is the story of the early days of the R.A.F. when Winston Churchill commanded the fledgling air force. Bill is sent to help fight the Bolsheviks in the Baltic where he has to learn to take-off
From Arctic Snow to Desert Sand
β Scribed by Hosker, Griff
- Book ID
- 109688942
- Publisher
- Sword Books Ltd
- Year
- 2017
- Tongue
- English
- Weight
- 566 KB
- Series
- British Ace 6
- Category
- Fiction
No coin nor oath required. For personal study only.
β¦ Synopsis
The novel takes Bill Harsker from the fields of France to other postings in the post war world of 1918. It is the story of the early days of the R.A.F. when Winston Churchill commanded the fledgling air force. Bill is sent to help fight the Bolsheviks in the Baltic where he has to learn to take-off and land on a carrier. There he has to learn how to play politics with men whose loyalties are not obvious. Ordered to the rebellion in Egypt and then Somaliland, Bill has to learn a whole range of new skills. Based upon actual events Arctic Snow to Desert Sand is the story of how the Royal Air Force learned its skills of war in a time of peace.
ES Index : 6
Number of Words in Auth: 2
Formats : EPUB
Number of Formats : 1
Has Cover : Yes
All Identifiers : goodreads:34757818, mobi-asin:cb0c4262-79f1-4162-be5d-c543c2c9f780
Test Text Series Index: Ace
Single Author : Griff Hosker
Original Source : MIRC Files_New_01_06
Sorted Author by LN, FN: Hosker, Griff
Title Length : 031
Title Parm D : From Arctic Snow to Desert Sand
Title Parm F : From Arctic Snow to Desert Sand
Num of Aut : 1
Title Parm B : (
Record ID : 673
Template Work Area : Ace
ES Name : British Ace
Uncomma Author : Griff Hosker
Title Parm A : From Arctic Snow to Desert Sand
π SIMILAR VOLUMES
Transportation, sublimation and accumulation of snow dominate snow cover development in the Arctic and produce episodic high evaporative Β―uxes. Unfortunately, blowing snow processes are not presently incorporated in any hydrological or meteorological models. To demonstrate the application of simple