acclimate
发表于 2025-3-23 11:37:20
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cruise
发表于 2025-3-23 15:06:09
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无法取消
发表于 2025-3-23 21:05:44
Textbook 1989nd nicht wirklich konsistent eingeführt werden. Auch beschränkt sich die Darstellung auf solche Konzepte, die unmittelbar dem Verständnis existierender experimenteller Beobachtungen dienen. Das Skript entstand nach und nach aus den Vorbereitungen für die Vorle sungen. Ohne dies ursprünglich zu beab
凹槽
发表于 2025-3-24 01:51:52
the examples and problems in the book are solved using the open-source Python programming language..Thebook will provide students in geothermal energy courses with a solid understanding of the subject. It will also be a valuable reference for professionals working in the field of renewable energy..978-3-031-32178-8978-3-031-32176-4
Ruptured-Disk
发表于 2025-3-24 05:28:23
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狗窝
发表于 2025-3-24 06:48:33
Fritz W. Boppn at an elementary level, but the interested reader is guided to the literature on splines.The concept of affine transformations, at the core of CAD software, is introduced in chapter 4, which includes applications of these transformations to the synthesis of curves and surfaces that would be extrem
弄皱
发表于 2025-3-24 11:55:43
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inquisitive
发表于 2025-3-24 17:01:46
Fritz W. Boppcause of the smallness of the vertical components of the Coriolis acceleration as compared to the gravity acceleration. In this case, the vector .. in the equations of motion is replaced by ...sin. (where . is the unit vector in the direction opposite to ., while . is the latitude of the observation
关心
发表于 2025-3-24 20:12:53
Fritz W. Boppame order of magnitude, equal to 1000 km (or 100 km respectively), although the square of their ratio (../..). is usually assumed to be equal to 0.1 with some reservations. This circumstance is related to one of the main difficulties in constructing an analytical theory of the general atmosphere and
说笑
发表于 2025-3-25 02:38:44
Fritz W. Bopp first study the linear stability of two-dimensional flows of an incompressible stratified fluid in a gravity field without taking into account the Coriolis forces. The results, as we shall see below, can be easily generalized to the global baroclinic geophysical flows. As a bonus, assuming the flui