|
|
|
|
| LEADER |
01000caa a22002652 4500 |
| 001 |
NLM252204816 |
| 003 |
DE-627 |
| 005 |
20250219012644.0 |
| 007 |
tu |
| 008 |
231224s2013 xx ||||| 00| ||eng c |
| 028 |
5 |
2 |
|a pubmed25n0840.xml
|
| 035 |
|
|
|a (DE-627)NLM252204816
|
| 035 |
|
|
|a (NLM)26311916
|
| 040 |
|
|
|a DE-627
|b ger
|c DE-627
|e rakwb
|
| 041 |
|
|
|a eng
|
| 100 |
1 |
|
|a Schwarz, J P
|e verfasserin
|4 aut
|
| 245 |
1 |
0 |
|a Global-scale seasonally resolved black carbon vertical profiles over the Pacific
|
| 264 |
|
1 |
|c 2013
|
| 336 |
|
|
|a Text
|b txt
|2 rdacontent
|
| 337 |
|
|
|a ohne Hilfsmittel zu benutzen
|b n
|2 rdamedia
|
| 338 |
|
|
|a Band
|b nc
|2 rdacarrier
|
| 500 |
|
|
|a Date Revised 08.04.2022
|
| 500 |
|
|
|a published: Print-Electronic
|
| 500 |
|
|
|a Citation Status Publisher
|
| 520 |
|
|
|a [1] Black carbon (BC) aerosol loadings were measured during the High-performance Instrumented Airborne Platform for Environmental Research Pole-to-Pole Observations (HIPPO) campaign above the remote Pacific from 85°N to 67°S. Over 700 vertical profiles extending from near the surface to max ∼14 km altitude were obtained with a single-particle soot photometer between early 2009 and mid-2011. The data provides a climatology of BC in the remote regions that reveals gradients of BC concentration reflecting global-scale transport and removal of pollution. BC is identified as a sensitive tracer of extratropical mixing into the lower tropical tropopause layer and trends toward surprisingly uniform loadings in the lower stratosphere of ∼1 ng/kg. The climatology is compared to predictions from the AeroCom global model intercomparison initiative. The AeroCom model suite overestimates loads in the upper troposphere/lower stratosphere (∼10×) more severely than at lower altitudes (∼3×), with bias roughly independent of season or geographic location; these results indicate that it overestimates BC lifetime
|
| 650 |
|
4 |
|a Journal Article
|
| 650 |
|
4 |
|a AeroCom
|
| 650 |
|
4 |
|a HIPPO
|
| 650 |
|
4 |
|a aerosol
|
| 650 |
|
4 |
|a black carbon
|
| 650 |
|
4 |
|a remote
|
| 650 |
|
4 |
|a tropical tropopause layer
|
| 700 |
1 |
|
|a Samset, B H
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Perring, A E
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Spackman, J R
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Gao, R S
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Stier, P
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Schulz, M
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Moore, F L
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Ray, Eric A
|e verfasserin
|4 aut
|
| 700 |
1 |
|
|a Fahey, D W
|e verfasserin
|4 aut
|
| 773 |
0 |
8 |
|i Enthalten in
|t Geophysical research letters
|d 1984
|g 40(2013), 20 vom: 28. Okt., Seite 5542-5547
|w (DE-627)NLM098182501
|x 0094-8276
|7 nnns
|
| 773 |
1 |
8 |
|g volume:40
|g year:2013
|g number:20
|g day:28
|g month:10
|g pages:5542-5547
|
| 912 |
|
|
|a GBV_USEFLAG_A
|
| 912 |
|
|
|a SYSFLAG_A
|
| 912 |
|
|
|a GBV_NLM
|
| 912 |
|
|
|a GBV_ILN_350
|
| 951 |
|
|
|a AR
|
| 952 |
|
|
|d 40
|j 2013
|e 20
|b 28
|c 10
|h 5542-5547
|