<div>The July 31 eruption of Steamboat was estimated at 200-300 feet high and the water phase lasted for approximately 9 minutes</div>
<div> </div>
<div>Denise Herman<br><br></div>
<div class="gmail_quote">On Sun, Aug 18, 2013 at 1:00 PM, <span dir="ltr"><<a href="mailto:geysers-request@lists.wallawalla.edu" target="_blank">geysers-request@lists.wallawalla.edu</a>></span> wrote:<br>
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<br>When replying, please edit your Subject line so it is more specific<br>than "Re: Contents of Geysers digest..."<br><br><br>Today's Topics:<br><br> 1. Re: Norris & Steamboat datastream... (Michael Goldberg)<br>
2. Re: Steamboat 7/31/13 @ 1940 (<a href="mailto:hi-plains@juno.com">hi-plains@juno.com</a>)<br> 3. Re: Norris & Steamboat datastream... (Ralph Taylor)<br><br><br>----------------------------------------------------------------------<br>
<br>Message: 1<br>Date: Thu, 15 Aug 2013 20:55:37 -0400 (EDT)<br>From: Michael Goldberg <<a href="mailto:goldbeml@ucmail.uc.edu">goldbeml@ucmail.uc.edu</a>><br>To: Geyser Observation Reports <<a href="mailto:geysers@lists.wallawalla.edu">geysers@lists.wallawalla.edu</a>><br>
Subject: Re: [Geysers] Norris & Steamboat datastream...<br>Message-ID:<br> <<a href="mailto:alpine.OSX.2.00.1308152041380.68191@ucfsb.ucfilespace.uc.edu">alpine.OSX.2.00.1308152041380.68191@ucfsb.ucfilespace.uc.edu</a>><br>
Content-Type: TEXT/PLAIN; charset=US-ASCII; format=flowed<br><br>I was curious about that temparature drop too.<br><br>The cloudburst explanation makes the most sense to me; also it fits in<br>with the prounounced spike in water flow at the Tantalus Creek stream<br>
gage: <a href="http://waterdata.usgs.gov/mt/nwis/uv?site_no=06036940" target="_blank">http://waterdata.usgs.gov/mt/nwis/uv?site_no=06036940</a><br><br>As for Steamboat's long-period cycles of minor activity, I couldn't agree<br>
more with your assessment!<br><br>Michael Goldberg<br><a href="mailto:Michael.Goldberg@uc.edu">Michael.Goldberg@uc.edu</a><br><br>On Thu, 15 Aug 2013, Davis, Brian L. wrote:<br><br>><br>>> The major eruption does not stick out as dramatically as one might expect.<br>
><br>> It doesn't... but there's some interesting things there anyway. A while<br>> back I posted that Steamboat had a long-period (weakfish, more like 5<br>> days currently I think) "envelope", with a resting or quiescent phase<br>
> every so often based on the stream temperatures. The major occurred on<br>> the first active period just after one of these quiescent phases, which<br>> may be significant, or a complete coincidence. If Steamboat would only<br>
> be kind enough to erupt in majors perhaps 10 more times, so that we<br>> could determine the correlation, that would be fine, thank you :).<br>><br>> I've been watching the graphs to see when it might start minor behavior<br>
> again (it hasn't apparently), an noticed something else odd - not at<br>> Steamboat, but at nearly every other instrumented Norris spot, there was<br>> a sudden temperature drop on the evening of 9 Aug. Porkchop, Opalescent<br>
> Spring, Constant, Echinus, all show this - but when I look at the Nuphar<br>> Lake air temperature, there is *not* a huge drop (but there *is* a<br>> drop... and there's a drop in the Vixen ground temperature, but later in<br>
> time than for the geyser runoff channels). Even things like the Gray<br>> Lakes show this downward spike very clearly. So a question for those who<br>> might know... was there one *heck* of a sudden downburst out there that<br>
> flooded everything with cold rainwater for a very brief time? And if so,<br>> does it surprise anyone else that it shows up almost not at all at<br>> Steamboat (where the channel sensor presumably has been dry or sitting<br>
> in a stagnant pool, and so I'd expect to see a strong response to a<br>> sudden downburst of cold rain)?<br>><br>> --<br>> Brian Davis<br>> _______________________________________________<br>> Geysers mailing list<br>
> <a href="mailto:Geysers@lists.wallawalla.edu">Geysers@lists.wallawalla.edu</a><br>> <a href="https://lists.wallawalla.edu/mailman/listinfo/geysers" target="_blank">https://lists.wallawalla.edu/mailman/listinfo/geysers</a><br>
><br><br><br>------------------------------<br><br>Message: 2<br>Date: Sat, 17 Aug 2013 16:00:03 GMT<br>From: "<a href="mailto:hi-plains@juno.com">hi-plains@juno.com</a>" <<a href="mailto:hi-plains@juno.com">hi-plains@juno.com</a>><br>
To: <a href="mailto:geysers@lists.wallawalla.edu">geysers@lists.wallawalla.edu</a><br>Subject: Re: [Geysers] Steamboat 7/31/13 @ 1940<br>Message-ID: <<a href="mailto:20130817.110003.28724.2@webmail15.vgs.untd.com">20130817.110003.28724.2@webmail15.vgs.untd.com</a>><br>
Content-Type: text/plain; charset=windows-1252<br><br>>> On Wed, 31 Jul 2013, David Monteith wrote:<br>>> Not much info yet but Steamboat was seen by Rosa Prasser at 1940 on July 31, 2013<br><br>Any info concerning height/duration, et al??<br>
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<br><br>------------------------------<br><br>Message: 3<br>Date: Sat, 17 Aug 2013 01:47:07 -0400<br>From: "Ralph Taylor" <<a href="mailto:ralpht@fuse.net">ralpht@fuse.net</a>><br>To: "'Geyser Observation Reports'" <<a href="mailto:geysers@lists.wallawalla.edu">geysers@lists.wallawalla.edu</a>><br>
Subject: Re: [Geysers] Norris & Steamboat datastream...<br>Message-ID: <009401ce9b0d$35ff7fa0$a1fe7ee0$@<a href="http://fuse.net/" target="_blank">fuse.net</a>><br>Content-Type: text/plain; charset="us-ascii"<br>
<br>If the sensor is uncovered and exposed to the sun a pronounced diurnal cycle<br>will be evident also.<br><br>Ralph Taylor<br><br>-----Original Message-----<br>From: <a href="mailto:geysers-bounces@lists.wallawalla.edu">geysers-bounces@lists.wallawalla.edu</a><br>
[mailto:<a href="mailto:geysers-bounces@lists.wallawalla.edu">geysers-bounces@lists.wallawalla.edu</a>] On Behalf Of Gordon Bower<br>Sent: Thursday, August 15, 2013 6:34 PM<br>To: Geyser Observation Reports<br>Subject: Re: [Geysers] Norris & Steamboat datastream...<br>
<br>Brian Davis wrote:<br><br>> noticed something else odd - not at Steamboat, but at nearly every other<br>instrumented Norris spot, there was a sudden temperature drop on the evening<br>of 9 Aug. Porkchop, Opalescent Spring, Constant, Echinus, all show this -<br>
but when I look at the Nuphar Lake air temperature, there is *not* a huge<br>drop (but there *is* a drop... and there's a drop in the Vixen ground<br>temperature, but later in time than for the geyser runoff channels). Even<br>
things like the Gray Lakes show this downward spike very clearly. So a<br>question for those who might know... was there one *heck* of a sudden<br>downburst out there that flooded everything with cold rainwater for a very<br>
brief time?<br><br>I was camping just outside the park, and there were several thunderstorms<br>the afternoon and evening of the 9th. It is possible.<br><br>>And if so, does it surprise anyone else that it shows up almost not at<br>
>all at Steamboat (where the channel sensor presumably has been dry or<br>sitting in a stagnant pool, and so I'd expect to see a strong response to a<br>sudden downburst of cold rain)?<br><br>The afternoon of the 10th, Steamboat's runoff channel was indeed dry, with<br>
rain puddles lingering in some of the deeper holes. It wasn't having minors<br>yet, and Cistern Spring was still out of sight, boiling and sloshing.<br><br>If the sensor is high and dry, it's only going to see a similar sized drop<br>
as the Nuphar Lake sensor as the air cools; if it's in a stagnant pool, the<br>pool is already near air temperature, and perhaps already full of rainwater<br>from an earlier shower. It doesn't have as far to drop as a sensor in a hot<br>
place does.<br><br>Without knowing exactly where the sensor is, all we can do is speculate.<br><br>_______________________________________________<br>Geysers mailing list<br><a href="mailto:Geysers@lists.wallawalla.edu">Geysers@lists.wallawalla.edu</a><br>
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<br>End of Geysers Digest, Vol 2672, Issue 1<br>****************************************<br></blockquote></div><br>