Return-path: X-Spam-Personal-Checker-Version: SpamAssassin 3.2.5 (2008-06-10) on chain.digitalkingdom.org X-Spam-Checker-Version: SpamAssassin 3.2.5 (2008-06-10) on chain.digitalkingdom.org X-Spam-Level: X-Spam-Status: No, score=-2.6 required=5.0 tests=AWL,BAYES_00 autolearn=ham version=3.2.5 Envelope-to: rlpowell@digitalkingdom.org Delivery-date: Fri, 14 Aug 2009 10:51:28 -0700 Received: from chain.digitalkingdom.org ([64.81.66.169]) by chain.digitalkingdom.org with esmtp (Exim 4.69) (envelope-from ) id 1Mc0vp-0005mw-72; Fri, 14 Aug 2009 10:51:17 -0700 Received: with ECARTIS (v1.0.0; list jbovlaste); Fri, 14 Aug 2009 10:50:32 -0700 (PDT) Received: from nobody by chain.digitalkingdom.org with local (Exim 4.69) (envelope-from ) id 1Mc0v5-0005mX-N1 for jbovlaste-real@lojban.org; Fri, 14 Aug 2009 10:50:32 -0700 Received: from mail-yw0-f172.google.com ([209.85.211.172]) by chain.digitalkingdom.org with esmtp (Exim 4.69) (envelope-from ) id 1Mc0v0-0005kT-NY for jbovlaste@lojban.org; Fri, 14 Aug 2009 10:50:27 -0700 Received: by ywh2 with SMTP id 2so2824386ywh.2 for ; Fri, 14 Aug 2009 10:50:16 -0700 (PDT) DKIM-Signature: v=1; a=rsa-sha256; c=relaxed/relaxed; d=gmail.com; s=gamma; h=domainkey-signature:mime-version:received:in-reply-to:references :date:message-id:subject:from:to:content-type :content-transfer-encoding; bh=iI840BIEiBhmQ6Sesod8g3eoutVFV8M3n2MWmj88Dlc=; b=fWpiBxNswd2xwtRSlgD0x1RTsffZwOELVe5z1VLYRfx2teZzncyNy/BFMrwx7cdS3x lhSERh9aNoANxn28ARLhm0afAkULx3F0pQl8Hk0gDd4iVHJzFwKeTTkbpBZ8p7uMizvh Rp4T5aKKzh47CnJOzj1I8UylE/DRbrZdsEnXk= DomainKey-Signature: a=rsa-sha1; c=nofws; d=gmail.com; s=gamma; h=mime-version:in-reply-to:references:date:message-id:subject:from:to :content-type:content-transfer-encoding; b=utOncCUeFpFtLz5JS7Eqszef3b8Th2yTS1I6JueNX8xlDefXsXbG6GeL64uUZhg2/v 8Jn8JfHFO7cbDvSw59PaNDcmqMnJK9DedTFDFUZajCDKrUX/YotEccHINnVou5afQLrc I8UsSVlGVj6Lmthi4SJSP9RQOMu4P1lKf17Bo= MIME-Version: 1.0 Received: by 10.151.9.9 with SMTP id m9mr2828718ybi.262.1250272216401; Fri, 14 Aug 2009 10:50:16 -0700 (PDT) In-Reply-To: <4de8c3930908111633t70fa8100u9c70a627b8c2e624@mail.gmail.com> References: <4de8c3930908111633t70fa8100u9c70a627b8c2e624@mail.gmail.com> Date: Fri, 14 Aug 2009 13:50:16 -0400 Message-ID: <96f789a60908141050l7c255608j43024d359e92c766@mail.gmail.com> Subject: [jbovlaste] Re: from core to exosphere From: Michael Turniansky To: jbovlaste@lojban.org Content-Type: text/plain; charset=UTF-8 Content-Transfer-Encoding: 8bit X-MIME-Autoconverted: from quoted-printable to 8bit by Ecartis X-ecartis-version: Ecartis v1.0.0 Sender: jbovlaste-bounce@lojban.org Errors-to: jbovlaste-bounce@lojban.org X-original-sender: mturniansky@gmail.com Precedence: bulk Reply-to: jbovlaste@lojban.org X-list: jbovlaste Content-Length: 2004 Lines: 49 On Tue, Aug 11, 2009 at 7:33 PM, tijlan wrote: Huh? Why moi in all the following? Also, despite the fact that your definitions are generic, your notes only refer to the Earth (in regards to the altitudes, etc.). And if only Earth has them, why do the even need the X2, x3 places? > > flemomvacri (troposphere) > $f_1=v_1$ is the troposphere (the lowest layer of atmosphere) of > planet/moon $v_2$, of composition $x_3$. > Notes: From 0 to 17 km in altitude. The Earth's troposphere contains > approximately 75 percent of the atmosphere's mass and 99 percent of > its water vapor and aerosols. Cf. {vacri}. > > dukmomvacri (stratosphere) > $d_1=v_1$ is the stratosphere (the second layer of atmosphere) of > planet/moon $v_2$, of composition $x_3$. > Notes: From 17 to 50 km in altitude. It is stratified in temperature, > with warmer layers higher up and cooler layers farther down. This is > in contrast to the troposphere. Cf. {vacri}. ??? How can an atmosphere be emotionally wrought? If you looking for physical turmoil, perhaps you should be looking at se jilca or kalsa? > > mijmomvacri (mesosphere) > $m_1=v_1$ is the mesosphere (the third layer of atmosphere) of > planet/moon $v_2$, of composition $x_3$. > Notes: From 50 to 85 in altitude. Cf. {vacri}. > > glamomvacri (thermosphere) > $g_1=v_1$ is the thermosphere (the fourth layer of atmosphere) of > planet/moon $v_2$, of composition $x_3$. > Notes: From 85 to over 640 km in altitude. The highly diluted gas in > this layer can reach 2,500 °C (4532°F) during the day. Cf. {vacri}. > > barmomvacri (exosphere) > $b_1=v_1$ is the exosphere (the uppermost layer of atmosphere) of > planet/moon $v_2$, of composition $x_3$. > Notes: From 500-1000 up to 10,000 km in altitude. In the exosphere, an > upward travelling molecule can escape to space if it is moving fast > enough to attain escape velocity; otherwise it will be pulled back to > the celestial body by gravity. Cf. {vacri}. > --gejyspa