<?xml version="1.0" encoding="utf-8" standalone="yes"?>
<rss version="2.0" xmlns:atom="http://www.w3.org/2005/Atom">
  <channel>
    <title>Environment on Shreyas Mandre</title>
    <link>https://www.shreyasmandre.com/tags/environment/</link>
    <description>Recent content in Environment on Shreyas Mandre</description>
    <generator>Hugo -- gohugo.io</generator>
    <language>en-us</language>
    <lastBuildDate>Sun, 10 Jan 2016 00:00:00 +0000</lastBuildDate><atom:link href="https://www.shreyasmandre.com/tags/environment/index.xml" rel="self" type="application/rss+xml" />
    <item>
      <title>Waving marine grass</title>
      <link>https://www.shreyasmandre.com/research/wavinggrass/</link>
      <pubDate>Mon, 04 Jan 2016 06:08:23 +0000</pubDate>
      
      <guid>https://www.shreyasmandre.com/research/wavinggrass/</guid>
      <description>&lt;p&gt;I bet you have seen gusts of wind exciting synchronized waves on the surface of tall grass field just like observed on the beach.&lt;/p&gt;</description>
    </item>
    
    <item>
      <title>Linear stability analysis for monami in a submerged seagrass bed</title>
      <link>https://www.shreyasmandre.com/publications/singh2016/</link>
      <pubDate>Sun, 10 Jan 2016 00:00:00 +0000</pubDate>
      
      <guid>https://www.shreyasmandre.com/publications/singh2016/</guid>
      <description>The onset of monami – the synchronous waving of seagrass beds driven by a steady flow – is modelled as a linear instability of the flow. Unlike previous works, our model considers the drag exerted by the grass in establishing the steady flow profile, and in damping out perturbations to it. We find two distinct modes of instability, which we label modes 1 and 2. Mode 1 is closely related to Kelvin–Helmholtz instability modified by vegetation drag, whereas mode 2 is unrelated to Kelvin–Helmholtz instability and arises from an interaction between the flow in the vegetated and unvegetated layers.</description>
    </item>
    
  </channel>
</rss>
