30 Minutes Rain Sounds Mp3 Download |BEST|

[Harold Guildford]

<div>My apologies for the delays. Chiming in to ensure everything is covered here. To confirm, are you hearing a different track or rain sound when you ask the Google Assistant on your phone to play it? I tried it on my end and was able to hear and play the same track. For the duration, for Google Home/Nest speakers the relaxing sound will continue to play for 12 hrs. unless you ask it to stop. You can try to reboot your device first and see if that makes any difference, or try using the keywords: "Hey Google, play rain sounds for ."</div><div></div><div></div><div></div><div></div><div></div><div>30 minutes rain sounds mp3 download</div><div></div><div>Download Zip: https://t.co/b2tB3uyBx4 </div><div></div><div></div><div>I use the sound skill at bed time and I'll get up at 2 am or so and the sounds have stopped, but the next morning I'll connect to my bluetooth speaker and it'll be playing still. It's not something that bothers me, but I was wondering if it happens to anyone else.</div><div></div><div></div><div>I've been using the Google Home Mini to help me sleep for the last 3 years or so. Each night I say "play rain and thunder" and then google will play relaxing rain noises for an hour and repeat until I turn it off which is great.</div><div></div><div></div><div>Tonight though, I can't get Google to play the rain noises for any longer than 10 minutes?!? He'll stop at 10 minutes and then repeat the track for another 10 minutes. Quite annoying and no idea why this has started now?</div><div></div><div></div><div>So, whether you want to drift off to dreamland for a restful slumber, want to heal an anxious mind, need a rainy day symphony to better meditate or want rain music to help you focus, work or study, this episode if perfect for you.</div><div></div><div></div><div>Welcome to Rainy Mood, the internet's most popular rain experience.</div><div></div><div></div><div></div><div>Millions of people use Rainy Mood while sleeping, studying, and relaxing.</div><div></div><div></div><div></div><div>Enjoy the free web version, or try the iOS/Android app with additional features.</div><div></div><div></div><div></div><div></div><div></div><div></div><div>Our longest duration rain stick, the XL Amaranth is the premiere choice as a sleep aid given its soft, soothing white(ish) noise and extra long duration. Enjoy 18-20 minutes of sustained rain sound as 4 million organically grown amaranth seeds descend down the wooden spiral. The Extra Large size creates a deeper pitched sound than our smaller offerings.</div><div></div><div></div><div>I wake up in the middle of the night and get on my phone (a habit I'm trying to break). I use my rainstick at that time. Instead of reaching for my phone I activate my rainstick and I go back to sleep within 15 minutes. I also use it as I'm winding down to go to sleep. It's well made and it's beautiful. So happy I made the investment.</div><div></div><div></div><div>Noah's beautiful rainsticks incorporate natural materials like amaranth (a small ancient grain) as the fill material for softer rain sounds, and clear micro glass beads for louder rain sounds. The simulated rain sound acts as a soothing and consistent background white noise that can bring the nervous system and mind into greater relaxation. And unlike other rainsticks on the market, these ingenious rainsticks were designed for much longer playing time, and stand up on their own ends without the need to hold it in your hands during play.</div><div></div><div></div><div>Spiral Rainsticks are perfect for personal relaxation and meditation at home, for teaching online or in person yoga and meditation, for including in sound baths, and also wonderful for audio recordings as well! As you can see, the rainsticks are visually striking, with the clear body allowing you to take in the sacred geometry of the continuous spiral through the center, and the meditative movement of the contents slowly moving from the top compartment to the bottom, grain by grain, seed by seed, bead by bead. An amazing addition to any healing instrument collection!</div><div></div><div></div><div>Like an hourglass, once the rainstick is placed upright with most or all the contents in the top compartment, gravity brings the contents through a small opening and a continuous amount of grains, seed or beads cascade down the internal bamboo or wooden spiral staircase, creating a prolonged gentle rain sound. The sound duration for each Spiral Rainstick depends on the rainstick size and the rainstick contents.</div><div></div><div></div><div>NEW! Portable Playing Stands now available! Highly recommended accessory to your Spiral Rainstick is the portable rainstick stand to keep your rainstick upright and balanced on any surface, indoor or out. Comes apart for transport and looks amazing</div><div></div><div></div><div>If you easily fall asleep when it's raining outside, then you'll love this one. It puts me right to sleep. Just say, "Alexa, play rain sounds" and your Echo will immediately conjure up the sound of a shower.</div><div></div><div></div><div>If you want to fall asleep to a different sound every night, this is a good skill to use. It has over 125 sounds to choose from, including thunderstorms, ocean sounds and crickets. When you're ready for a snooze, just say "Alexa, tell Sleep Sounds to play thunderstorms," or whatever sound you want to hear. You can set a sleep timer so it won't play all night by saying "Alexa, set a sleep timer for three hours."</div><div></div><div></div><div>Not everyone can sleep in a pitch-black room, but a TV can be distracting when you're trying to snooze. If all you need is a little light, then put your Echo's ring light to use. Just say "Alexa, open night light" and the top of your Echo will start glowing and pulsing. It'll glow for five minutes unless you give it a specific amount of time.</div><div></div><div></div><div>Rain and Thunder Sounds 10 minutes. Rain Drops Loop Sound Effect. Rain Noise Sounds. Rain Sound for Sleeping. Sound of Rain Falling. Relaxing Rain Noise. Rain Sounds. Rain Sound Effects. Rainy Mood. Sleep Sounds. Free Mp3 Downloads.</div><div></div><div></div><div>There are a number of ways to use rain sounds for sleep, including listening to rain audio recordings or using a rain machine that emits the sound of falling rain. Studies have shown that the sound of rain can help to slow down heart rate and breathing, which can lead to improved sleep quality.</div><div></div><div></div><div>Another way to control the volume of rain sounds is to use an app on your smartphone or tablet. There are many different apps that play rain sounds at different volumes so you can find one that suits your needs.</div><div></div><div></div><div>Another option is to search for rain sounds online. There are usually many different videos to choose from, and you can often find ones that are an hour or longer. You can also look for rain sounds on nature sound websites. These websites usually have a wide selection of sounds, including rain, that you can download and listen to offline.</div><div></div><div></div><div>Finally, if you have a smartphone or other mobile device, there are many apps that offer rain sounds with additional features like a bedtime reminder and fade-out timer to help you relax and fall into a deep sleep.</div><div></div><div></div><div>Start by finding a spot where you can record without too much background noise. Once you have your recording device set up, simply let the rain do its work. You may want to experiment with different positions and angles in order to get the best sound quality.</div><div></div><div></div><div>There are a few things to keep in mind if you want to get the most out of using rain sounds for sleep. First, make sure to find a recording that has a consistent sound throughout; nothing is more jarring than a loud clap of thunder in the middle of the night!</div><div></div><div></div><div>Dr. Miyamoto suggests planning ahead by going to bed slightly earlier for a few days before the switch. This will help you adjust to the time change and hold you accountable for setting up a more consistent sleep schedule. He also suggests getting 15 minutes of sunlight exposure early in the day to help reset your circadian clock.</div><div></div><div></div><div>This rainmaker in the form of a pillar produces a sound like a fine summer rain and, depending on its size, lasts from 2 to 22 minutes without having to be turned over again. Listening to this sound calms, relaxes and harmonizes and has a soothing effect on heart and mind</div><div></div><div></div><div>What are some of the disadvantages of the Skew-T Log-P diagrams:Available generally twice a day (00Z and 12Z), character of weather can change dramatically between soundings. Sounding does not give a true vertical dimension since wind blows balloon downstream Sounding does not give true instantaneous measurements since it takes several minutesto travel from the surface to the upper troposphere</div><div></div><div></div><div>This section interprets most of those values and gives operational significance to the values. Each parameter orindice will be broken down one by one. In a severe weather situations and during inclement weather, these indices come in handy. The indices should be used as guides. Often, indices will contradict each other and can change rapidly in the course of a couple of hours. An experienced meteorologist is well informed to how a sounding will change throughout the day and why some sounding indices are better than others in certain situations. Soundings are most notably changed through thermal advection, moisture advection, and evaporational cooling. Modified soundings should be studied along with the standard 12Z and 00Z sounding.</div><div></div><div></div><div></div><div> </div><div></div><div></div><div></div><div>(BRN) - Bulk Richardson Number</div><div></div><div> EQUATION: (CAPE / 0-6km shear)</div><div></div><div> less than 45 (Supercells) less than 10 (Environment too sheared) Teens (Optimum for severe storms, good balance of CAPE and shear)</div><div></div><div>(BSHR) - Bulk shear value (magnitude of shear over layer).</div><div></div><div></div><div></div><div>(CAP) - Cap strength in degrees Celsius. Values above 2 indicate convectionwill not occur within at least the next couple of hours. Cap needs to be less than 2 in general before it can bebroken.</div><div></div><div></div><div></div><div>(CAPE) - Convective Available Potential Energy. This is the positive area on asounding (the area between</div><div></div><div> theparcel and environmental temperature). </div><div></div><div> 1 to 1,500 (Positive CAPE) 1,500 to 2,500 (Large CAPE) 2,500+ (Extreme CAPE)</div><div></div><div> Max upward vertical velocity = (2*CAPE)^1/2, does not take into consideration water loading, entrainment. Largest CAPE will occur in the warm sector of a mid-latitude cyclone High values of CAPE will result in high values of upward vertical velocity in the updraft region of a thunderstorm CAPE is increased by low level warm air advection, daytime heating, low level moisture advection (highlow level dewpoint), upper level cold air advection (cooling temperature in mid-levels) CAPE values tend to be highest in the warm season (especially late Spring)</div><div></div><div>(CCL) - Convective Condensation Level. Level at which condensation will occur if sufficient afternoonheating causes rising parcels of air to reach saturation. The CCL is greater than or equal in height (lower or equal pressure level) than the LCL. The CCL and the LCL are equal when the atmosphere is saturated. Found at the intersection of the saturation mixing ratio line (through the surface dewpoint) and the environmental temperature.</div><div></div><div></div><div></div><div>(CIN) - Convective Inhibition. This is the negative area on a sounding. A large cap or a dry planetaryboundary layer will lead to high values of CIN and stability.</div><div></div><div></div><div></div><div>Convective instability - Occurs when a dry layer overlays a warm and humid layer. Lifting of atmosphere causes the lapse rate to increase since the lower layer cool at the WALR while the dry layer cools at the DALR.</div><div></div><div></div><div></div><div>Convective Temperature - The approximate temperature that the air near the ground must warm to in order for surface-based convection to develop, based on analysis of a sounding. Calculation involves many assumptions, such that thunderstorms sometimes develop well before or well after the convective temperature is reached (or may not develop at all). However, in some cases the convective temperature is a useful parameter for forecasting the onset of convection. Also-the convective temperature is found on a Skew-T Log-P diagram by dropping a parcel of air dry adiabatically from the CCL (Convective Condensation Level) to the surface and reading off the new temperature once the parcel reaches the surface. </div><div></div><div></div><div></div><div>Think of the convective temperature as the temperature the surface of the earth must warm to in order forthunderstorms to occur in the absence of synoptic scale forcing mechanism (i.e., development of afternoon "air-mass" thunderstorms). The convectivetemperature is most likely to be reached in the late afternoon hours due to cumulative solar heating. The strength of the "cap" determines if the convective temperature will be reached. When the cap is very strong, the convective temperature will be higher than the high temperature for that dayand thus no storms develop. The amount of low level moisture also determines if the convective temperature will be reached. The CCL increases in height as the average PBL dewpoint decreases.A higher CCL results in a higher convective temperature. Dynamic upward forcing lowers the theoretical convective temperaturesince parcels of air can be "forced" or brought closer to the CCL by lifting mechanisms such as fronts, low level WAA and low level convergence.</div><div></div><div></div><div></div><div>(EHI) - Energy helicity index. Combines CAPE and Helicity into a single index. EHI increases as CAPE and/or Helicity increases. Tornadicdevelopment often initiates in region of EHI max (especially if EHI max is 5 or greater).</div><div></div><div></div><div></div><div>EQUATION: (SR HEL * CAPE) / 160,000 </div><div></div><div>EHI > 1 (Supercells likely)EHI from 1 to 5 (F2, F3 tornadoes possible)EHI 5+ (F4, F5 tornadoes possible)</div><div></div><div>(EI) - Energy Index</div><div></div><div></div><div></div><div>(EL) - Equilibrium level. The pressure value at the top of the positive CAPEarea In extreme situtations, EHI max will be near 10.</div><div></div><div></div><div></div><div>Equivalent Potential Temperature - Also known as THETA-E. Temperature of a parcel after all latent heat energy is released in a parcel then brought to the 1000 mb level. From pressure of interest (typically the surface) find the LCL, lift the parcel wet adiabatically to 100 mb. Next, descend the parcel dry. </div><div></div><div></div><div></div><div>(FRZ) - Pressure level at which the environmental sounding is exactly zero degrees Celsius. Find intersection of 0-degreeisotherm with environmental sounding.</div><div></div><div></div><div></div><div>(HEL) - Helicity Amount of streamwise vorticity available for ingestion into a storm. Streamwise vorticity is a function of low level inflow and horizontal vorticity generated by speed shear with height or directional shear with height in the PBL.</div><div></div><div>150 to 300 (possible supercell)300 to 400 (supercell severe storms)400+ (Tornadic supercells possible)</div><div></div><div>Low level inflow, speed shear and directional shear maximize helicity valuesHelicity values tend to be highest ahead of cold fronts and near warm fronts within the warm sector of a mid-latitude cycloneThe Low Level Jet can amplify low level inflow. Higher winds lead to a more rapid rotation of air if shear existsDifferential advection and surface friction cause speed and directional shear</div><div></div><div>Hydrolapse - Rapid increase or decrease in dewpoint with height.</div><div></div><div></div><div></div><div>(K) - K Index. The K Index is primarily applicable in the prediction of air mass thunderstorms. Low values of the K Index in the presence of other strong thunderstorms indicators (sharp trough, high level jet, etc.) may suggest a severe thunderstorm potential. For example, a low K value might result from a 700 mb dry tongue. Limitations: Favors non severe convection. This index is a measure of thunderstorm potential but has nothing to do with severity of storms. Can not be used in mountain areas. The K value may not be representative of the airmass if the 850mb level is near the surface.</div><div></div><div></div><div></div><div>EQUATION: (T850 - T500) + (Td850 - Td700)</div><div></div><div> Lapse rate + available moisture</div><div></div><div> -or-</div><div></div><div>EQUATION: (T850 - T500) + ( Td850 ) - (T700 - Td700)</div><div></div><div>(Lapse rate) + (low-level moisture) - (extent of moist layer)</div><div></div><div>mb thick. The mean temperature and relative humidity are used to determine the temperature and dewpoint of the parcel at 25 mb above the surface. Then the parcel is lifted dry-adiabatically to saturation, and moist adiabatically to 500 mb. This parcel temperature is subtracted from the initialized or forecast500 mb temperatures at each grid point to yield the MLI.</div><div></div><div></div><div></div><div>(MAXT) - Estimated maximum afternoon temperature. Most relevant when using a morning sounding. Most accurate on days with clear skies and moderate winds.</div><div></div><div></div><div></div><div>(MPL) - Maximum parcel level. Highest level a parcel can rise in the atmosphere. This value is above the EL due to the updrafts momentum.</div><div></div><div></div><div></div><div>(Potential Temperature) - Temperature found by lifting or descending a parcel to the 1000 mb level from the pressure level of interest.</div><div></div><div></div><div></div><div>(PW) - Value of precipitable water in inches. This is the amount of liquid water on the surface after all water in all three phases is brought to the surface.</div><div></div><div>Greater than 1.75 inches represents a water loaded sounding. Less than 0.75 inches represents a fairly dry sounding.</div><div></div><div>(RH) - Relative Humidity. Found by dividing the mixing ratio by the saturation mixing ratio or the vapor pressure divided by the saturation vapor pressure. Find the saturation mixing ratio value that runs through the dewpoint and the temperature. Next, divide the dewpoint mixing ratio by the temperature mixing ratio. The average relative humidity between the surface and 500 millibars. Relative humidity is a good measure of the evaporational drying power of the air and how close the atmosphere is to saturation. It does not, however, tell you how much moisture mass there is in the air. Adiabatically to the 1000 mb level. The temperature at 1000 mb of this parcel is the THETA-E.</div><div></div><div>0 to 40% (very low)41 to 60% (low)61 to 80% (moderate)81 to 100% (moist)</div><div></div><div>(SHR) - Positive shear in the 0 to 3000m above ground level. Units are in time to the negative 1. Dividing the change in vertical wind speed by the change in the distance derives these units. Km/hr divided by km = hr-1. Value is found by finding the change in wind speed from the surface to 3000m and dividing that value by 3000m (3 km). </div><div></div><div>0 to 3 (weak)4 to 5 (moderate)6 to 8 (large) 9+ (very large)</div><div></div><div>(SI) - Showalter Index. Same as LI, except parcel is lifted from 850 mb. Use SI instead of LI in the cool season especially when surface is capped by a cool front.</div><div></div><div></div><div></div><div>EQUATION: 500 mb environmental temperature - 500 mb parcel temperature</div><div></div><div>A. Lift the 850 mb temperature dry adiabatically until it intersects the mixing ratio line which passes through the 850 mb dewpoint.</div><div></div><div>B. Lift the parcel moist adiabatically to 500 mb. </div><div></div><div>C. The difference between the ambient air temperature at 500 mb and the parcel temperature determines the SI.</div><div></div><div></div><div></div><div>(SRDS) - Storm relative directional shear.</div><div></div><div></div><div></div><div>(STM) - Estimated storm motion. Storm will be moving from X and X knots.</div><div></div><div></div><div></div><div>(SWEAT) - Severe WEAther Threat Index. Indice combining many thermodynamic and wind values.The SWEAT Index was developed by AWS to indentify areas of potentially severe convective activity. The terms in the index refer to low level moisture, convective potential, lowand mid level winds, and wind shear. Empirically, the threshold for severe thunderstorms is 300 and the threshold for tornadoes is 400. It should be stressed that the above statistics were derived from known severe weather cases; nothing can be inferred above the false alarm ratio. Also, the SWEAT Index gives severe weather potential; a trigger is still needed to realize this potential. this SWI should not be used to predict ordinary thunderstorms. Since this index can change dramatically in a short period of time, it should be computed at both 12Z and 00Z during severe weather situations. Formula covers: low level moisture, instability, low level jet, upper level jet, warm airadvection</div><div></div><div>150 to 300 (Slight severe)300 to 400 (Severe storms possible)400+ (Tornadic severe storms possible)</div><div></div><div>(T</div>