Controlled weather balloon ascents and descents for atmospheric research and climate monitoring

Kräuchi, Andreas; Philipona, Rolf; Romanens, Gonzague; Hurst, Dale F.; Hall, Emrys G.; Jordan, Allen F.

doi:https://doi.org/10.5194/amt-9-929-2016

Articles | Volume 9, issue 3

Atmos. Meas. Tech., 9, 929–938, 2016

https://doi.org/10.5194/amt-9-929-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Atmos. Meas. Tech., 9, 929–938, 2016

https://doi.org/10.5194/amt-9-929-2016

© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 9, issue 3

Research article

07 Mar 2016

Research article | 07 Mar 2016

Controlled weather balloon ascents and descents for atmospheric research and climate monitoring

Andreas Kräuchi et al.

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Dec 2015	64	54	2	120
Jan 2016	44	19	0	63
Feb 2016	26	16	0	42
Mar 2016	138	94	3	235
Apr 2016	34	38	3	75
May 2016	20	15	0	35
Jun 2016	11	9	2	22
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Aug 2016	17	15	1	33
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Oct 2016	12	23	0	35
Nov 2016	9	19	0	28
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Jan 2017	16	15	0	31
Feb 2017	10	15	0	25
Mar 2017	15	31	2	48
Apr 2017	24	41	1	66
May 2017	35	33	1	69
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Aug 2017	13	27	1	41
Sep 2017	15	43	1	59
Oct 2017	13	44	0	57
Nov 2017	15	45	0	60
Dec 2017	15	30	1	46
Jan 2018	6	29	0	35
Feb 2018	6	31	1	38
Mar 2018	15	46	1	62
Apr 2018	21	51	0	72
May 2018	20	46	1	67
Jun 2018	20	50	3	73
Jul 2018	10	47	0	57
Aug 2018	24	69	0	93
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Oct 2018	14	40	0	54
Nov 2018	9	46	0	55
Dec 2018	13	31	0	44
Jan 2019	17	29	0	46
Feb 2019	12	21	0	33
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Apr 2019	15	35	1	51
May 2019	14	28	0	42
Jun 2019	11	26	0	37
Jul 2019	8	23	0	31
Aug 2019	8	34	0	42
Sep 2019	15	38	2	55
Oct 2019	19	28	1	48
Nov 2019	4	27	0	31
Dec 2019	16	40	1	57
Jan 2020	13	28	1	42
Feb 2020	14	15	0	29
Mar 2020	9	15	0	24
Apr 2020	8	15	0	23
May 2020	18	30	0	48
Jun 2020	21	16	1	38
Jul 2020	40	32	13	85
Aug 2020	16	14	8	38
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Oct 2020	16	13	1	30
Nov 2020	12	14	0	26
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Jan 2021	20	17	0	37
Feb 2021	17	29	0	46
Mar 2021	22	37	1	60
Apr 2021	25	38	1	64
May 2021	18	29	1	48
Jun 2021	20	29	2	51
Jul 2021	12	19	1	32
Aug 2021	14	21	3	38
Sep 2021	20	17	0	37
Oct 2021	13	49	1	63
Nov 2021	17	36	3	56
Dec 2021	25	23	0	48
Jan 2022	13	24	0	37
Feb 2022	16	18	0	34
Mar 2022	31	21	0	52
Apr 2022	28	25	4	57
May 2022	14	13	1	28
Jun 2022	14	12	0	26

Cumulative views and downloads (calculated since 03 Dec 2015)

Month	HTML	PDF	XML	Total
Dec 2015	64	54	2	120
Jan 2016	44	19	0	63
Feb 2016	26	16	0	42
Mar 2016	138	94	3	235
Apr 2016	34	38	3	75
May 2016	20	15	0	35
Jun 2016	11	9	2	22
Jul 2016	13	8	2	23
Aug 2016	17	15	1	33
Sep 2016	15	14	0	29
Oct 2016	12	23	0	35
Nov 2016	9	19	0	28
Dec 2016	5	10	0	15
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Feb 2017	10	15	0	25
Mar 2017	15	31	2	48
Apr 2017	24	41	1	66
May 2017	35	33	1	69
Jun 2017	32	22	2	56
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Aug 2017	13	27	1	41
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Dec 2017	15	30	1	46
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Apr 2018	21	51	0	72
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Feb 2019	12	21	0	33
Mar 2019	9	38	0	47
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May 2019	14	28	0	42
Jun 2019	11	26	0	37
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Jan 2020	13	28	1	42
Feb 2020	14	15	0	29
Mar 2020	9	15	0	24
Apr 2020	8	15	0	23
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Jul 2020	40	32	13	85
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Oct 2020	16	13	1	30
Nov 2020	12	14	0	26
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Feb 2021	17	29	0	46
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May 2021	18	29	1	48
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Oct 2021	13	49	1	63
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Dec 2021	25	23	0	48
Jan 2022	13	24	0	37
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Mar 2022	31	21	0	52
Apr 2022	28	25	4	57
May 2022	14	13	1	28
Jun 2022	14	12	0	26

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Latest update: 30 Jun 2022

Short summary

In situ upper-air measurements are often made with instruments attached to weather balloons launched at the surface and lifted into the stratosphere. It has been demonstrated that ascending weather balloons can perturb the air measured by very sensitive humidity and temperature sensors trailing behind them. The use of controlled balloon descent for such measurements has therefore been investigated and is described here. We present two different methods and show advantages and disadvantages.

Article

Controlled weather balloon ascents and descents for atmospheric research and climate monitoring

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Cited

10 citations as recorded by crossref.

10 citations as recorded by crossref.

Saved (final revised paper)

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