找回密碼
 To register

QQ登錄

只需一步,快速開始

掃一掃,訪問微社區(qū)

打印 上一主題 下一主題

Titlebook: Aeolian Grain Transport; The Erosional Enviro Ole E. Barndorff-Nielsen,Brian B. Willetts Conference proceedings 1991 Springer-Verlag Wien 1

[復制鏈接]
樓主: aggression
31#
發(fā)表于 2025-3-27 00:14:25 | 只看該作者
32#
發(fā)表于 2025-3-27 02:40:07 | 只看該作者
Air flow and sand transport over sand-dunes,d different sets of measurements over a dune, by Howard and Walmsley [5], and by our group in recent field measurements over a dune in Oman, and in a new wind-tunnel study of Howard’s dune. It is found that the FLOWSTAR calculations agree well with these sets of measurements upwind of the brink. Sin
33#
發(fā)表于 2025-3-27 07:29:38 | 只看該作者
Cross-shore selective sorting processes and grain size distributional shape, along the -0.6 to -0.7 . lines. However, this group is divided into two basically different depositional environments: water-lain backshore populations dominated by the swash-backwash bidirectional sheet flow and wind-blown sand originating from the backshore sediments. The different grain-size pop
34#
發(fā)表于 2025-3-27 11:20:17 | 只看該作者
Assessment of aerodynamic roughness via airborne radar observations,sensitivity of the relationship to microwave parameters using calibrated multiple wavelength, polarization, and incidence angle aircraft radar data, and 3) applying the results to models to gain an understanding of the physical properties which produce the relationship. The approach combines the mea
35#
發(fā)表于 2025-3-27 17:26:54 | 只看該作者
36#
發(fā)表于 2025-3-27 19:35:48 | 只看該作者
The effect of sea cliffs on inland encroachment of aeolian sand,he beach parallel to the foot of the cliff represents the effect of a non-homogeneous secondary wind. The wind is accelerated along the cliff, and as a result sand transport increases along the cliff. After a length of 150-200 m along the front slopes of the cliffs a state of equilibrium is achieved
37#
發(fā)表于 2025-3-28 00:48:22 | 只看該作者
38#
發(fā)表于 2025-3-28 02:10:17 | 只看該作者
39#
發(fā)表于 2025-3-28 06:36:03 | 只看該作者
Ergebnisse der empirischen Untersuchung, along the -0.6 to -0.7 . lines. However, this group is divided into two basically different depositional environments: water-lain backshore populations dominated by the swash-backwash bidirectional sheet flow and wind-blown sand originating from the backshore sediments. The different grain-size pop
40#
發(fā)表于 2025-3-28 11:36:24 | 只看該作者
https://doi.org/10.1007/978-3-8349-9969-6sensitivity of the relationship to microwave parameters using calibrated multiple wavelength, polarization, and incidence angle aircraft radar data, and 3) applying the results to models to gain an understanding of the physical properties which produce the relationship. The approach combines the mea
 關(guān)于派博傳思  派博傳思旗下網(wǎng)站  友情鏈接
派博傳思介紹 公司地理位置 論文服務流程 影響因子官網(wǎng) 吾愛論文網(wǎng) 大講堂 北京大學 Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點評 投稿經(jīng)驗總結(jié) SCIENCEGARD IMPACTFACTOR 派博系數(shù) 清華大學 Yale Uni. Stanford Uni.
QQ|Archiver|手機版|小黑屋| 派博傳思國際 ( 京公網(wǎng)安備110108008328) GMT+8, 2025-10-14 08:49
Copyright © 2001-2015 派博傳思   京公網(wǎng)安備110108008328 版權(quán)所有 All rights reserved
快速回復 返回頂部 返回列表
华阴市| 东港市| 通州区| 永兴县| 东至县| 汝州市| 大邑县| 米脂县| 黄浦区| 栾川县| 庆阳市| 合水县| 东海县| 洛南县| 白山市| 台中市| 白山市| 任丘市| 三河市| 左云县| 博白县| 宜宾市| 宁远县| 华蓥市| 巨野县| 马边| 铅山县| 原阳县| 黔西| 大新县| 泽州县| 岳阳县| 沙雅县| 万安县| 潼关县| 兴业县| 高邮市| 宁阳县| 百色市| 凭祥市| 钟山县|