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How would I run a command then immediately close the terminal?

How would I run a command in Terminal then immediately close the Terminal window?
I usually do:
screen -R /path/to/my/program/my/command


screen -ls
Display list of open screens.
screen -r
Attach to the given screen, if it is running. This is the same as
the -R option. The -X option detaches.

So you could do:
screen -R /path/to/my/program/my/command

which works with both the interactive and detached (tmux) modes.


Try using screen and tmux together.
With tmux you can run something like this:
tmux run-program ssh server-id “open -a /Applications/Google\”

to launch Google Chrome and see the results.


tmate is a much simpler to use “Terminal Multiplexer”.
set/unset terminal features;
prompt $*

Effective actions: encouraging patients to quit smoking.
Smokers between the ages of 18 and 65 who are eligible to participate in the Medicare and Medicaid programs are included in an ongoing demonstration project in which pharmacists deliver brief intervention to smokers during routine visits in group practice settings. Over 90 percent of smokers receiving pharmacists’ intervention have had a quit attempt within three months of the intervention. Rates of successful quit attempts are as high as 55 percent. The project

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Ansys V14 for Windows 32 bit en-ger-jp-fr MAGNiTUDE 16 torrent. ANSYS 16.0 On CNET Download page for an easy, fast, 24/7. Ansys 16.0 On CNET Download page for an easy, fast, 24/7.*=0.92) and *mcrA* transcript abundance (log~10~) (*r*=0.57) ([Fig. 5b](#fig5){ref-type=”fig”}). Based on these results, *mcrA* transcript abundance is a better proxy for measured methanogenesis rates than enzyme activity.


It is shown here that functional methanogenesis is active during hydrothermal carbonate alkalinity blanketing of mussel shells, in a brine-dominated system at the D’Orbigny Vent Field. The ability to measure carbon dioxide emissions with a membrane-based total-carbon dioxide concentration system and to detect autotrophic carbon fixation at the site is also demonstrated. These are first direct observations of methanogenesis in serpentinized settings. Methanogenesis thus appears to have the potential to contribute significantly to C~1~ mineralization during low temperature serpentinization. The addition of CO~2~ (e.g., calcite dissolution by fluid mixing or partial CO~2~ adsorption by calcite and other minerals) and H~2~ (e.g., serpentinization) could explain the persistent detection of methanogenesis in mussel shell carbonate.

Although deep-brine CH~4~ fluxes in other systems can be measured using similar methods,^[@cit24],[@cit55]^ this is only the second reported example where CH~4~ fluxes can be detected from an open system. Geochemical measurements demonstrate that methanogenesis is occurring at a vent field on the Juan de Fuca Ridge where there is no direct evidence of active hydrothermal circulation.^[@cit56]^

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